1997–98 South Pacific cyclone season: Difference between revisions

Category 3 severe tropical cyclone (Australian scale)
Category 3 tropical cyclone (SSHWS)
Duration	October 27 – November 5
Peak intensity	155 km/h (100 mph) (10-min);; 945 hPa (mbar)

Category 2 tropical cyclone (Australian scale)
Tropical storm (SSHWS)
Duration	October 8 – October 12
Peak intensity	100 km/h (65 mph) (10-min);; 980 hPa (mbar)

1997–98 South Pacific cyclone season
1997–98 South Pacific cyclone season
	Season summary map
Seasonal boundaries
First system formed	October 8, 1997
Last system dissipated	May 3, 1998
Strongest storm
Name	Ron and Susan
• Maximum winds	230 km/h (145 mph); (10-minute sustained)
• Lowest pressure	900 hPa (mbar)
Seasonal statistics
Total depressions	20
Tropical cyclones	16 (record high)
Severe tropical cyclones	7
Total fatalities	50 total
Total damage	> $7.6 million (1998 USD)
Related articles
	1997–98 Australian region cyclone season; 1997–98 South-West Indian Ocean cyclone season;
	South Pacific tropical cyclone seasons; 1995–96, 1996–97, 1997–98, 1998–99, 1999–00

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The 1997–98 South Pacific cyclone season was the most active and longest South Pacific tropical cyclone seasons on record, with 16 tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. The season started earlier than normal with 3 systems developing before the official start of the season on November 1, 1997, while the final system of the season dissipated on May 3, 1998, after the season had officially ended on April 30. During the season 50 people died as a result of tropical cyclones, with the deadliest being Cyclone Martin with 27 known deaths. The strongest tropical cyclones during the season were Cyclone Ron and Cyclone Susan as both were estimated to have minimum pressures of 900 hPa (26.58 inHg), and were the most intense tropical cyclones on record in the South Pacific Ocean until Cyclone Zoe in 2002–03. After the season ended, 11 names had their names either removed or retired from the lists of names, after they caused significant impacts to South Pacific islands.

During the season, tropical cyclones were officially monitored by the Regional Specialized Meteorological Center (RSMC) in Nadi, Fiji and the Tropical Cyclone Warning Centers in Brisbane, Australia and Wellington, New Zealand. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) and Naval Pacific Meteorology and Oceanography Center (NPMOC), also monitored the basin and issued unofficial warnings for American interests. During the season RSMC Nadi issued warnings and assigned names to any tropical cyclones that developed between the Equator and 25°S while TCWC Wellington issued warnings for any that were located to the south of 25°S. The JTWC issued warnings for American interests on any significant tropical cyclone that was located between 160°E and the 180° while the NPMOC issued warnings for tropical cyclones forming between 180° and the American coast. RSMC Nadi and TCWC Wellington estimated sustained windspeeds over a 10-minute and used the Australian tropical cyclone intensity scale, while the JTWC and the NPMOC estimated sustained windspeeds over a 1-minute period which are compared to the Saffir-Simpson Hurricane Scale (SSHS).

Seasonal outlooks

Record	Tropical Cyclone	Severe Tropical Cyclone	Ref
Average activity: (1969–70 – 1996–97)	7 – 8	4	^[1]
Record high activity:	1982-83: 14	1982–83:10	^[2]
Record low activity	1994–95: 3	1994–95: 0	^[2]
Activity during this season:	16	7	^[3]

Ahead of the season officially starting on November 1, the American Samoan Governor reported that traditionalists were forecasting a hurricane to affect American Samoa, during the season after the big breadfruit and mango harvest that the island nation had experienced.^[4] The Cook Islands Meteorological Service and National Disasters Committee warned islanders that they could expect the "worst cyclone season in years."^[5] On November 27, New Zealand's National Institute of Water and Atmospheric Research, issued a press release, which predicted that because of the strong El Niño phenomenon, there would be more tropical cyclones than average.^[6] In particular they predicted that due to the strong El Niño, countries within the western part of the basin were likely to see fewer tropical cyclones during the season than countries within the eastern part of the basin.^[6]

The Southern Cook Islands, Tonga, Tuvalu and French Polynesia, were predicted to have an increased risk, while Fiji was forecast to have an average risk of being affected by a tropical cyclone.^[6] NIWA also reported that Cyclone Martin's impact on the Northern Cook Islands was an early sign of what could be expected during the season, because the system had occurred further east than normal.^[6] In mid December the Cook Islands Meteorological Service director commented to the media that from now on, by the time cyclones reached Raro-Tonga would have lost their intensity, while a spokesperson for NIWA commented that holidaymakers heading for the Pacific had a little chance of running into a cyclone as the damaging core of the cyclone was expected to be over the ocean while some cyclones were expected to be relatively weak.^[7] It was also noted that collectively the Pacific Islands Meteorological Services were bracing for up to 15 tropical cyclones during the season, compared to 12 during an average season.^[7]

Seasonal summary

The 1997–98 season was one of the most active and longest South Pacific tropical cyclone seasons on record, with 16 tropical cyclones occurring within the South Pacific basin between 160°E and 120°W.^[8] The season was characterised by a very strong El Niño Event, which caused the South Pacific Convergence Zone, to move from its usual position near the Solomon Islands to the Northern Cook Islands.^[1] As a result, ten tropical cyclones formed to the east of the International Dateline, with seven of these tropical cyclones going on to affect French Polynesia.^[1] After the 1996-97 season had one of the latest ends to a season on record, the 1997-98 season started early with three tropical systems observed before the start of the season on November 1, 1997.^[8] Two other tropical systems, including the precursor tropical disturbance to Severe Tropical Cyclone Martin developed, before the official start of the season on November 1, 1997.^[9] Severe Tropical Cyclone Martin impacted the Cook Islands and French Polynesia, where it caused significant damage and 28 deaths during the opening days of the season.^[9] Tropical Cyclone Nute was named on November 18, before it moved out of the basin as a Category 2 tropical cyclone during November 19.^[10] During the rest of November, several tropical disturbances developed along the South Pacific Convergence Zone, including the precursor system to Severe Tropical Cyclone Osea and Tropical Cyclone Pam.^[10]^[11] Osea was named

Severe Tropical Cyclones Ron and Susan were both the strongest tropical cyclones of the season and were thought to be the strongest tropical cyclones in the region since Severe Tropical Cyclone Hina of the 1984-85 season.^[1]

After the final warnings on Cyclone Tui were issued a weak circulation remained in the vicinity of Samoa for several days, before a westerly surge from the monsoon resulted in a tropical cyclone developing during February 1.^[1] However, due to uncertainties in the continuation of Tui after several other weak low pressure areas had formed, RSMC Nadi decided to treat the cyclone as a separate system and named it Wes.^[12]

Tropical Cyclone Bart developed during the final days of the season and caused ten deaths and minor damage to French Polynesia, before it dissipated during May 3. The names Katrina, Martin, Nute, Osea, Ron, Susan, Tui, Ursula and Veli, were subsequently retired from the lists of names for the region.^[13]

Systems

Tropical Cyclone Lusi

On October 4, a cyclonic circulation became evident within an area of convection, that was located about 500 km (310 mi) to the southeast of Yaren in Nauru.^[14]^[15] Over the next few days the system moved southwards, towards the upper subtropical ridge while outflow gradually developed further.^[14]^[15] During October 8, the system was classified as a tropical depression as the system rapidly developed further, before the JTWC initiated initiated advisories on the depression and designated it as Tropical Cyclone 02P.^[9]^[16]^[17] The FMS subsequently named the depression Lusi during the next day, as the system had intensified into the earliest tropical cyclone since 1970, while located about 1,020 km (635 mi)^* to the northwest of Port Villa, Vanuatu.^[9]^[18]^[19] Over the next few days, Lusi moved towards the south-southeast, taking a so-called "gentleman's track" between Vanuatu and Fiji.^[8]

During October 10, the JTWC reported that Lusi had peaked with 1-minute sustained wind speeds of 110 km/h (70 mph), while the system was located about 570 km (355 mi)^* to the northwest of Port Vila, Vanuatu.^[15] The FMS subsequently followed suit during the next day and estimated peak 10-minute sustained wind speeds of 100 km/h (65 mph).^[18] After it had peaked in intensity Lusi started to weaken in an area of cooler sea surface temperatures, while vertical windshear increased because of a mid level trough and strong north-westerlies.^[8]^[14] During October 12, Lusi degenerated into an extratropical cyclone, before the remnants were last noted to the northeast of New Zealand^[9]^[15]^[20] There was no impact caused by Lusi on any island, however, widespread heavy rainfall and gale force wind speeds were reported on several Fijian Islands.^[17]

Severe Tropical Cyclone Martin

On October 27, the FMS started to monitor a weak tropical disturbance that had developed to the north of the Northern Cook Islands.^[8] Over the next few days atmospheric convection surrounding the system remained disorganised, as the system moved to the southwest and was affected by strong upper-level north-easterly winds and moderate to strong vertical wind shear.^[1]^[9] Late on October 30, the NPMOC designated the disturbance as Tropical Cyclone 04P, after it had developed into a tropical depression.^[9]^[21]^[22] During the next day the system started to show a marked improvement in organisation and began rapidly developing, before RSMC Nadi named it Martin at 1500 UTC after it had developed into a category 1 tropical cyclone.^[8] When it was named, Martin was located about 500 km (310 mi)^* to the west of Manihiki Atoll in the Northern Cook Islands and had started to re-curve and move towards the south-east during that day.^[8]^[20]^[23] Early on November 1, RSMC Nadi reported that the system had become a category 2 tropical cyclone on the Australian scale, before the NPMOC reported that Martin had become equivalent to a category 1 hurricane on the SSHWS.^[20]^[24]

During November 2, the system continued to intensify as it moved towards the southeast and became equivalent to a category 2 hurricane on the SSHWS, as it moved towards the French Polynesian Society Islands of Bellingshausen, Mopelia and Scilly.^[1]^[20]^[24] During the next day, Martin passed near the Society Islands as it developed an 17 km (10 mi)^* eye, before RSMC Nadi reported at 06:00 UTC that the system had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind speeds of 155 km/h (100 mph).^[1]^[18]^[25] The NPMOC also reported at around that time that Martin had peaked with 1-minute sustained windspeeds of 185 km/h (115 mph), which made it equivalent to a category 3 hurricane on the SSHWS.^[24]^[25] After peaking in intensity Martin started to weaken, as it interacted with a frontal system and started to accelerate towards the south-southeast.^[8]^[26] During November 4, Martin passed within 250 km (160 mi) of Tahiti as it became a category 2 tropical cyclone and started to transition into an extratropical cyclone.^[8]^[18]^[27] Later that day, the NPMOC issued their final advisory on system as it had become equivalent to a tropical depression, vertically sheared with its surface center dislocated about 110 km (70 mi)^* from its upper level center.^[24]^[28] During November 5, Martin weakened below tropical cyclone intensity as it moved into TCWC Wellington's area of responsibility before the system was last noted on November 8.^[8]^[20]

Tropical Cyclone Nute

Category 2 tropical cyclone (Australian scale)
Category 1 tropical cyclone (SSHWS)

Duration	November 18 – November 19
Peak intensity	110 km/h (70 mph) (10-min); 975 hPa (mbar)

On November 15, the United States Armed Forces started to monitor a tropical disturbance, that had developed within the South Pacific Convergence Zone about 1000 km (620 mi) to the northeast of Suva, Fiji.^[29]^[30] Over the next few days the system moved towards the west, before it came under the influence of the subtropical ridge of high pressure.^[29]^[30] At 0000 UTC on November 18, RSMC Nadi reported that the system had become a tropical depression, before the JTWC issued a tropical cyclone formation alert on the depression while it was located about 100 km (60 mi), to the southwest of the Solomon Island: Santa Cruz.^[31]^[32] The JTWC initiated advisories on the depression at 0600 UTC and designated it as 05P, before six hours later, RSMC Nadi named the depression Nute, as it had intensified into a category one tropical cyclone.^[8]^[32] Over the next day, Nute continued to intensify and developed an eye feature before at 0600 UTC on November 19, as the system approached 160°E, RSMC Nadi reported that Nute, had peaked as a category two tropical cyclone with 10-minute sustained wind speeds of 110 km/h (70 mph).^[8]^[31] During that day RSMC Nadi reported that Nute was holding on to its peak intensity, while the JTWC reported at 1800 UTC that Nute had reached its 1-minute peak intensity of 140 km/h (85 mph) as it was entering the Australian region.^[10]^[29] As Nute traversed an island-free area of the western South Pacific, there were no deaths or impact reported.^[31]

Severe Tropical Cyclone Osea

Category 3 severe tropical cyclone (Australian scale)
Category 2 tropical cyclone (SSHWS)

Duration	November 22 – November 28
Peak intensity	150 km/h (90 mph) (10-min); 950 hPa (mbar)

On November 22, RSMC Nadi started to monitor a tropical depression that had developed about 465 km (290 mi)^* to the northeast of Manihiki Island.^[10]^[33] Over the next two days, the depression gradually developed further.^[10]^[34] At 1200 UTC on November 23, the NPMOC reported that the depression had become equivalent to a tropical storm and assigned it the designation 06P, before 12 hours later RSMC Nadi named the system Osea as it had developed into a category 1 tropical cyclone.^[8]^[34] After developing into a tropical cyclone, Osea started moving towards the southeast.^[10]^[35] During November 26, both agency's reported that the system had reached its peak intensity, with RSMC Nadi reporting 10-minute sustained windspeeds of 150 km/h (90 mph), while the NPMOC reported peak 1-minute sustained windspeeds of 165 km/h (105 mph).^[20]^[33] After it had peaked, Osea started to gradually weaken, before during November 27 the NPMOC issued their final warning on the system as it had become sheared.^[36] RSMC Nadi subsequently monitored Osea for another 24 hours before the system degenerated into a depression during November 28.^[8]^[20]

While it was active, Osea caused no deaths but was quite destructive to some of the northwestern Society Islands, with over 700 homes destroyed or severely damaged on Maupiti, Bora-Bora, and Raiatea.^[1] On Maupiti, an island with a population of 1,100, about 95% of the infrastructure was destroyed. The town hall, two schools, and an airfield were destroyed.^[37] The town hall was evacuated due to the strong winds.^[38] In addition, 77 homes on the island were destroyed.^[39] Due to flooding, many highways were blocked.^[40] On Bora-Bora, an island which had a population of 4,500 at the time, roughly 30% of the infrastructure was destroyed, including 309 houses.^[10] On the north side of Bora Bora, nearly everything was destroyed, including the village of Vaitape.^[41] In Vaitape, roads were blocked and telecommunication lines were hampered. Seven people on the island were injured.^[42]^[43] Overall, 700 homes were at least somewhat destroyed by Osea.^[44] Throughout French Polynesia, banana trees were knocked down due to the strong winds.^[45]

Tropical Cyclone Pam

Category 2 tropical cyclone (Australian scale)
Category 1 tropical cyclone (SSHWS)

Duration	December 6 – December 10
Peak intensity	110 km/h (70 mph) (10-min); 975 hPa (mbar)

At the end of November, an equatorial westerly wind burst, occurred about 2,000 km (1,245 mi)^* to the south-west of Hawaii. This wind burst led to the development of two tropical cyclones, to the east of the International Dateline on either side of the equator.^[1] During December 5, both RSMC Nadi and the NPMOC started to monitor the system as a tropical depression, while it was located between the Samoan and Northern Cook Islands.^[1]^[46]^[47] During that day the system slowly developed and organized further and moved south-eastwards, before early on December 6, RSMC Nadi reported that the system had developed into a category 1 tropical cyclone and named it Pam.^[8]^[46] After it was named the system continued to slowly drift towards the south-southeast, before it started to move quicker later that day as it passed near the Cook Island of Suwarrow.^[46] As the system passed near Suwarrow, the NPMOC reported that Pam had reached its peak intensity with 1-minute sustained wind speeds of 120 km/h (75 mph), which made it equivalent to a category 1 hurricane on the SSHWS.^[48]

Over the next couple of days the system moved southwards before RSMC Nadi reported during December 8, that Pam had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind-speeds of 120 km/h (75 mph)^*.^[46]^[49] However, during the systems post analysis, RSMC Nadi reduced these winds slightly to 110 km/h (70 mph)^* which made Pam a category 2 tropical cyclone, rather than a category 3 severe tropical cyclone on the Australian scale.^[20]^[49] During December 8, the system passed about 140 km (85 mi)^* to the east of Palmerston Island, before it passed about 75 km (45 mi)^* to the southwest of Rarotonga early the next day.^[46] During December 9, Pam started to rapidly weaken as it transitioned into an extra-tropical cyclone, while RSMC Nadi reported during the next day that the system had degenerated into depression.^[46]^[50] Over the next few days the system continued to move southeastwards, before it was last noted during December 14, while located to the west of Chile.^[20]

Severe Tropical Cyclone Susan

Category 5 severe tropical cyclone (Australian scale)
Category 5 tropical cyclone (SSHWS)

Duration	December 20 – January 9
Peak intensity	230 km/h (145 mph) (10-min); 900 hPa (mbar)

On December 20, RSMC Nadi started to monitor a weak tropical disturbance, that was located about to the north of Tuvalu.^[51]^[52] Over the next two weeks the system gradually moved towards the west-southwest, without developing into a tropical cyclone.^[51] During January 3, the JTWC initiated warnings on the system and designated it as Tropical Cyclone 11P.^[53] Later that day RSMC Nadi named the system Susan as the system had become a category 1 tropical cyclone, while it was located near the Fiji dependency of Rotuma.^[54] During that day the system continued to rapidly develop with RSMC Nadi reporting early on January 4, that Susan had become a category 3 severe tropical cyclone, with 10-minute sustained windspeeds of 120 km/h (75 mph).^[18] Later that day the JTWC reported that Susan had become equivalent to a category 1 hurricane on the Saffir-Simpson Hurricane Scale, as atmospheric convection surrounding the system organized further and developed an eye feature.^[52]^[55]

Susan subsequently moved towards the southwest as the subtropical ridge of high pressure weakened.^[56] Early on January 5, RSMC Nadi reported that Susan had peaked as a category 5 severe tropical cyclone with 10-minute sustained wind speeds of 140 mph (220 km/h), while the JTWC reported that Susan had peaked with 1-minute wind speeds of 260 km/h (160 mph) equivalent to a low-end category five hurricane on the SSHS.^[18]^[52]^[56] As the system reached its peak intensity, Susan was moving towards the southwest and as a result, it "posed a severe threat to Vanuatu," however during that afternoon, Susan recurved towards the southeast "just in time to spare Vanuatu, a direct hit.”^[8] After turning away from Vanuatu, Susan accelerated towards the southeast while remaining near or at its peak intensities, before starting to weaken significantly during January 7.^[18] RSMC Nadi then reported early the next day, that Susan had weakened into a category 4 severe tropical cyclone while it was located about 435 km (270 mi)^*, to the southeast of Nadi, Fiji, which was close enough for the system to produce gale force winds in several southern and western Fijian Islands.^[1]^[18] Later that day, Susan started to interact with Ron before by 0000 UTC on January 9, Susan had completely absorbed Ron.^[8] The final advisories on the combined system, were then released later that day as the system lost its tropical characteristics and started to undergo an extratropical transition.^[8]^[57] The remnants of the combined systems were then monitored for another day until they were last noted at 1200 UTC on January 10, bringing an unseasonable cold snap to New Zealand.^[20]^[58]

Total damage from Susan was minor.^[51] High seas in accordance with Susan inundated the village of Talaulia on Kadavu, Fiji. There was also some destroyed waterfront buildings, roads, jetties and bridges on Kadavu. In Beqa Island, only high seas and swells were experienced. In the town of Lautoka, on Viti Levu, roofs were blown off shops. This damage was possibly caused by a tornado that formed from one of the outer rain bands. One death was reported in accordance with Susan. This death was on Ambrym Island in Vanuatu, where a woman was killed by a falling coconut palm tree.^[51]

Severe Tropical Cyclone Ron

Category 5 severe tropical cyclone (Australian scale)
Category 5 tropical cyclone (SSHWS)

Duration	January 1 – January 8
Peak intensity	230 km/h (145 mph) (10-min); 900 hPa (mbar)

The first tropical depression advisory was released on January 1 at 600 UTC to a depression that was to become Tropical Cyclone Ron. Ron drifted slowly for the next four days and reached tropical cyclone intensity on January 2 near Samoa. As a cyclone, Ron passed close to Swains Island on January 3 and intensified gradually after that. Peak 10-minute winds of 145 mph (225 km/h) were reached on January 5 north of Apia, American Samoa. Ron maintained that intensity for about 36 hours and began to move in a south-southeasterly course on January 6. Around 1800 UTC that day, Ron passed near Niuafo'ou, which reported sustained winds of 70 mph (110 km/h). The RSMC Nadi discussion at 1800 UTC noted that Ron may have had a smaller gale radius than had been thought. After passing Niuafo'ou, Ron passed to the south of Samoa and weakened. Ron started to move faster and weakened rapidly, merging with Tropical Cyclone Susan on January 9. Ron's lowest pressure was 900 millibars and 1-minute winds of 165 mph (265 km/h).^[51]

Damage on Niuafo'ou was catastrophic. About 67 percent of the buildings on were either damaged or destroyed completely. Agricultural losses included 80–90 percent of the coconut and breadfruit trees were damaged. Crops such as taro, kape, manioc, and bananas were lost. The Tonga Chronicle reported that it would take at least five years to return crops to pre-cyclone stages. Damages and rehabilitation totaled out 1.1 million in Tongan dollars. However, no fatalities were reported on the island. Neighboring islands Niuatoputapu, Tafahi, and Vava'u sustained damage as well, but not as severe as Niuafo'ou. No reports of damage came from Swain's Island and Wallis Island. Ron's peak intensity of 900 millibars was the strongest of the season in the Southern Pacific and the strongest since Tropical Cyclone Hina in March 1985.^[51]

Severe Tropical Cyclone Katrina

Category 3 severe tropical cyclone (Australian scale)
Category 2 tropical cyclone (SSHWS)

Duration	January 7 – January 11
Peak intensity	150 km/h (90 mph) (10-min); 955 hPa (mbar)

During January 7, Cyclone Katrina moved into the basin as a Category 2 tropical cyclone, while it was located about 90 km (55 mi)^* to the south of the Solomon Island: Rennel.^[18]^[51] The system subsequently moved south-eastwards and intensified further, before it became a Category 3 Severe Tropical Cyclone and posed a threat to Vanuatu during the next day.

Tropical Cyclone Tui

Category 1 tropical cyclone (Australian scale)
Tropical storm (SSHWS)

Duration	January 25 – January 27
Peak intensity	75 km/h (45 mph) (10-min); 990 hPa (mbar)

On January 25, both RSMC Nadi and the NPMOC reported that Tropical Depression 16P, had developed about 360 km (225 mi) to the northwest of Apia, Samoa.^[8]^[18]^[22] During that day, as the depression moved towards the southeast it gradually intensified further before at 2100 UTC, RSMC Nadi reported that the depression had intensified into a category one tropical cyclone, and named it as Tui, while it was located about 80 km (50 mi) to the northwest of Apia.^[8] After it was named, Tui passed over the Samoan Islands of Upolu and Savai'i, before at 0600 UTC, both RSMC Nadi and the NPMOC reported that Tui had peaked with 10 and 1 minute sustained windspeeds of 75 km/h (45 mph).^[18]^[59] After it had crossed Samoa, the system remained near stationary, just to the south of Samoa, before early on January 27 both the NPMOC and RSMC Nadi, reported that Tui had weakened into a depression and issued their final advisories.^[8]^[51]^[59] After Tui was downgraded to a depression, a weak circulation remained in the vicinity of the Samoan islands for several days, before it possibly redeveloped into Tropical Cyclone Wes.^[1]^[8] Ahead of Tui affecting the Samoan islands, Polynesian Airlines and Samoa Air cancelled all of their flights to the islands.^[60] Large crop losses and some infrastructure damage were reported in American Samoa and Western Samoa after gale force wind gusts, heavy rain and rough seas brought down power lines, trees and other debris.^[61]^[62] On the Western Samoan island of Savai'i, a young boy was killed when he stepped into an electrified puddle of water.^[8]

Tropical Cyclone Ursula

Category 2 tropical cyclone (Australian scale)
Category 1 tropical cyclone (SSHWS)

Duration	January 29 – February 2
Peak intensity	110 km/h (70 mph) (10-min); 975 hPa (mbar)

Just after Tropical Cyclone Tui had weakened into a depression near the Samoan Islands, a new tropical depression developed to the northeast of Tahiti in French Polynesia during January 29.^[1] Over the next day the system subsequently moved south-eastwards and gradually developed further, before it was declared to be a Category 1 tropical cyclone and named Ursula by the FMS.^[51] Ursula subsequently gradually intensified and accelerated towards the south-east, as it got caught up in a westerly flow and passed through the Tuamotu archipelago.^[18] During February 1, the system peaked as a Category 2 tropical cyclone with 10-minute wind speeds of 110 km/h (65 mph), before the NPMOC initiated advisories and designated Ursula as Tropical Cyclone 17P with peak 1-minute wind speeds of 120 km/h (75 mph).^[18]^[51]^[63] Over the next day the system transitioned into an extratropical cyclone, before the remnants were last noted on February 5, while they were located around 4,350 km (2,705 mi)^* to the southwest of Lima, Peru.^[1]^[20] In association with Tropical Cyclone Veli, Ursula brought significant waves which caused minor damages to three Tuamotuan islands of Mataiva, Rangiroa, Makatea.^[64] Mataiva was the worst hit island with 39 homes damaged, while roads and bridges were washed away.^[64] On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted, after coral and sand washed up onshore.^[64]

Tropical Cyclone Veli

Category 2 tropical cyclone (Australian scale)
Category 1 tropical cyclone (SSHWS)

Duration	January 30 – February 3
Peak intensity	100 km/h (65 mph) (10-min); 980 hPa (mbar)

During January 30, a tropical depression developed about 650 km (405 mi)^* to the northeast of Apia in American Samoa.^[18] Over the next couple of days the system moved eastwards while gradually developing further, with the NPMOC issuing a tropical cyclone formation alert on the system early on February 1.^[18]^[65] Later that day the FMS named the system Veli as it had intensified into a category 1 tropical cyclone, while it came under the influence of a mid level trough of low pressure and started to move towards the southeast.^[65] Later that day the NPMOC started to issue warnings on the system and designated it as Tropical Cyclone 18P, after it had continued to organize and convection surrounding the system had increased.^[65] During that day Veli continued to move towards the southeast while gradually intensifying, before early the next day the NPMOC reported that the system had peaked with 1-minute sustained wind speeds of 140 km/h (85 mph).^[66] Veli peaked as a category 2 tropical cyclone early on February 2, with 10-minute sustained wind speeds of 100 km/h (65 mph).^[18] Over the next day, the cyclone moved through the Tuamotu group of islands, as it began to experience significant vertical windshear and weakened into a depression.^[67] The system was subsequently monitored until it was last noted during February 4, about 1,500 km (930 mi)^* to the northwest of Adamstown on the Pitcairn Islands.^[20] In association with Tropical Cyclone Ursula, Veli brought significant waves to French Polynesia's Tuamotu province and caused minor damages on the islands of Mataiva, Rangiroa, Makatea.^[64] Mataiva was the worst hit island with roads and bridges washed away, and 39 homes damaged.^[64] On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted after coral and sand washed up onshore.^[64]

Tropical Cyclone Wes

Category 2 tropical cyclone (Australian scale)
Tropical storm (SSHWS)

Duration	January 31 – February 5
Peak intensity	95 km/h (60 mph) (10-min); 985 hPa (mbar)

On January 31, the FMS reported that a tropical depression had developed, about 230 km (145 mi)^* to the northwest of the American Samoan island of Apia.^[12] During that day the depression moved slowly eastwards and intensified further, before it was named Wes by the FMS, after it had developed into a Category 1 tropical cyclone during February 1.^[12] The NPMOC subsequently designated it as Tropical Cyclone 19P and initiated advisories later that day, with peak 1-minute sustained wind speeds of 85 km/h (50 mph).^[12]^[68] The system subsequently continued to move eastwards and passed about 95 km (60 mi)^* to the south of the Cook Island: Nassau.^[1]^[12] During February 3, the FMS reported that the system had peaked, with 10-minute sustained wind speeds of 90 km/h (55 mph)^* which made it a category 2 tropical cyclone on the Australian scale.^[18] Later that day the system subsequently started to rapidly weaken as it moved into an area of higher vertical wind shear and interacted with the westerlies.^[69]^[70] The system was subsequently last noted during February 5, while located about 400 km (250 mi)^* to the east of Papeete, on the island of Tahiti, French Polynesia.^[12]^[18] The system did not directly affect any inhabited islands, while there was no damage reported on Suwarrow from the system.^[1] However, 10 people were killed on the French Polynesian island of Tahaa, after two days of heavy rain associated with Wes caused a landslide during February 6.^[71]^[72]

Severe Tropical Cyclone Yali

Category 3 severe tropical cyclone (Australian scale)
Category 2 tropical cyclone (SSHWS)

Duration	March 18 – March 25
Peak intensity	130 km/h (80 mph) (10-min); 965 hPa (mbar)

The system that was too become Yali was first noted as a tropical disturbance, to the northeast of Vanuatu during March 17.^[73]^[74] During that day atmospheric convection over the disturbance's low level circulation center became better defined, before the JTWC initiated advisories and designated the system as Tropical Cyclone 29P, while the system was located about 650 km (405 mi)^* to the north-northwest of Port Vila.^[8]^[75] Over the next day the system moved towards the west-southwest between Vanuatu and the Solomon Islands under the influence of the subtropical ridge of high pressure to the south of the system.^[76] RSMC Nadi subsequently reported late on March 19, that the system had developed into a category 1 tropical cyclone and named it Yali.^[8] After it was named Yali re-curved and started moving towards the south-southeast, as the monsoonal flow to the north of the system strengthened.^[8]^[75]

For the next 2½ days, Yali moved to the southeast, passing west of the Vanuatu Islands. Yali came close enough to affect the isles of Tanna and Aneityum. Yali reached hurricane-force on the afternoon of March 21 and passed 60 nautical miles (110 km) west of Port Vila the next day.^[75] Yali's peak intensity of 80 mph (130 km/h) and 965 millibars was reached on March 22 at 600 UTC.^[75] At this time, Yali was just south of Port Vila, brushing it with 15 mph (24 km/h) winds and a minimal pressure of 992 millibars. There was a possibility that the low wind reading based on poor exposure of the instrument. By 1800 UTC March 22, Yali reached its most easternmost position at 220 nautical miles (410 km) southeast of Port Vila. The upper ridge to its north intensified, increasing wind shear and limiting convection. Due to this, Yali began to weaken and dropped below hurricane force.^[75] At around the same time, a mid-level subtropical ridge began to influence its motion, sending it to the west. As Yali moved to the southwest, the wind field became asymmetric. At 1200 UTC March 23, Yali was just east of Noumea, New Caledonia with winds of 50 mph (80 km/h). The weakening Yali passed just south of New Caledonia on the night of March 23. By March 25, an upper-level low had caught the cyclone and influenced the circulation with cold air.^[75]

RSMC Nadi downgraded Yali into an extratropical system and stopped issuing advisories.^[75] The JTWC continued to track Yali in the general direction of Australia. The now semi-tropical Yali moved to the west and crossed 160°E on March 25. By the next day, Yali's center was 300 nautical miles (560 km) east-northeast of Brisbane, Australia. Some convection was re-developing just south of the center with gales possibly affecting the Australian coast on March 27. On the morning of March 27, the JTWC released its final bulletin on Yali, 325 nautical miles (602 km) east-southeast of Brisbane. The remnants of Yali went under a transformation in the Tasman Sea. The remnants came under a double jet structure and strong cyclone vorticity advection at 500 millibars.^[75] The remnants of Yali deepened and moved towards the southern end of New Zealand.^[75] The central pressure of the remnants reached 970–975 millibars as it crossed the coast of South Island on March 29. After passing New Zealand, Yali's remnants passed below the Antarctic Circle and was absorbed by a circumpolar trough between 65°S and 75°S.^[75] Tanna received rather severe damage from Yali, however monetary estimates are not available.^[75] About 60–70 percent of crops were destroyed and about 30% of the houses were damaged by the storm. Both Tanna and Aniwa were suffering a severe drought, so food stocks were low. Other places in Vanuatu only received minor damage. The passage of Yali in New Zealand caused high seas and flooding over South Island, Westport and Nelson. One fatality occurred when a youth died in New Plymouth. Trees toppled, roofs were ripped off and power lines fell.^[75]

Severe Tropical Cyclone Zuman

Category 3 severe tropical cyclone (Australian scale)
Category 3 tropical cyclone (SSHWS)

Duration	March 29 – April 5
Peak intensity	150 km/h (90 mph) (10-min); 955 hPa (mbar)

During March 29, the FMS started to monitor a tropical depression that had developed under an upper level ridge of high pressure, about 520 km (325 mi)^* to the northeast of Port Vila, Vanuatu.^[64]^[77] Over the next day the system quickly developed further as it slowly moved, towards Northern Vanuatu and was designated as Tropical Cyclone 31P early on March 30.^[64]^[78]

Tropical Cyclone Alan

Category 1 tropical cyclone (Australian scale)
Tropical storm (SSHWS)

Duration	April 17 – April 26
Peak intensity	75 km/h (45 mph) (10-min); 992 hPa (mbar)

On April 17, the FMS started to monitor a tropical disturbance, that had developed to the east of the Northern Cook Islands.^[8]^[79] Over the next few days the system moved erratically, before it developed into a Category 1 tropical cyclone and was named Alan by the FMS during April 21.^[8] When it was named the system was located about 300 km (185 mi)^* to the east-southeast of Manihiki and had started to move westwards.^[1] During April 22, the FMS estimated that Alan had reached its peak intensity with 10-minute sustained wind speeds of 75 km/h (45 mph), as the system started to pose several forecasting challenges as it was difficult to locate and estimate how intense the system was.^[1]^[20] Later that day the NPMOC started to issue warnings on Alan and estimated peak 1-minute sustained wind speeds of 85 km/h (50 mph).^[80]^[81] During April 23, the system appeared to become sheared with the low level circulation centre displaced about 20 km (10 mi)^* from the nearest atmospheric convection.^[1]^[82] As a result, the FMS reported that Alan had weakened into a depression, while the NPMOC issued their final advisory on the system.^[8]^[79]^[82] Over the next day as a mid level trough of low pressure that had been shearing the system moved faster than expected the depression became better organized.^[35]^[79]

As a result, the NPMOC initiated advisories on the system again during April 24, while the FMS reported that Alan had re-intensified into a category 1 tropical cyclone later that day.^[20]^[35] The system was now located about 555 km (345 mi)^* to the west-northwest of the French Polynesian island of Tahiti, and was now moving towards the south-southeast under the influence of an upper level anticyclone located to the east of Alan.^[35]^[79] Early on April 25, Alan passed near too or over the French Polynesian Society Islands of Maupiti, Bora-Bora, and Raiatea.^[79] During April 25, strong wind shear pulled the system apart, with visible imagery showing that the system had a fully exposed low level circulation.^[8] As a result, the FMS reported that the system had weakened into a depression at 1800 UTC that day, while it was located about 185 km (115 mi)^* to the west-northwest of Tahiti.^[8]^[79] The NPMOC subsequently reissued their final advisory early the next day, as the system drifted towards the south-southeast while located to the west of Tahiti.^[79]^[83] The system affected French Polynesia with high winds and torrential rain, which caused several landslides within the Society Islands.^[79]^[84] The landslides caused two bridges to collapse and along with fallen trees blocked roads.^[85] Overall ten people died as a result of the system while thirty others were injured, with the majority of the casualties occurring due to landslides.^[1]^[86] On the islands of Ra'iātea, Tahaa and Huahine several churches, schools and clinics were damaged while water and electricity supplies were cut off.^[1]^[85] Within the islands around 750 houses were destroyed with 430 and 150 of these occurring on Huahine and Ra'iātea respectively.^[85]

Tropical Cyclone Bart

Category 1 tropical cyclone (Australian scale)
Tropical storm (SSHWS)

Duration	April 28 – May 3
Peak intensity	85 km/h (50 mph) (10-min); 987 hPa (mbar)

During April 28, a tropical depression developed out of an area of low pressure, about 650 km (405 mi)^* to the northeast of Papeete, French Polynesia.^[8]^[18] Over the next 24 hours the depression moved quickly to the southeast, while gradually intensifying with nearby automatic weather stations reporting strong winds and significant pressure drops.^[8]^[87] The depression was subsequently named Bart by the FMS during April 29, after it had developed into a category 1 tropical cyclone on the Australian scale near the island of Hao.^[79]^[88] The FMS reported during the next day that Bart had reached its peak 10-minute sustained windspeeds of 85 km/h (50 mph), as the system slowed down due to a blocking ridge of high pressure strengthening.^[8]^[18]

The NPMOC subsequently initiated advisories on Bart and designated it as Tropical Cyclone 37P, while it was at its peak 1-minute sustained windspeeds of 65 km/h (40 mph).^[87]^[88] However, by this time Bart had started to weaken, before on May 1, satellite imagery showed that the systems, low level centre had become exposed as the main area of convection had become sheared.^[8] Despite gale force wind speeds occurring in Bart's southern semicircle, the system weakened into a tropical depression during May 1, before it dissipated to the north of Pitcairn Island on May 3.^[8]^[79]^[89] Minor damage was recorded in French Polynesia, while 10 deaths were associated with Bart after waves from the system capsized a boat.^[1]^[8]^[90]

Other systems

On October 24, the United States Armed Forces started to monitor an area of disturbed weather, that was located about 800 km (500 mi) to the north of Nadi, Fiji.^[91] Over the next couple of days the system moved towards the southwest before early on October 26, as convection surrounding the system organized further, the FMS reported that the system had developed into a tropical depression, while the JTWC issued a tropical cyclone formation alert on it.^[9]^[92] Later that day the JTWC initiated advisories on the depression designating it as Tropical Cyclone 03P, while it was at its peak 1-minute sustained windspeeds of 65 km/h (40 mph).^[91]^[92] Over the next couple of days, a trough of low pressure approached the system and caused the depression to move south-eastwards, before the system dissipated to the north west of Fiji during October 28.^[9] On February 11, a tropical depression developed about 185 km (115 mi) to the northwest of the Northern Cook Island: Suwarrow Atoll.^[12] Over the next couple of days the depression moved westwards slowly before the centre was relocated late on February 13 to a position about 185 km (115 mi) to the south-southeast of Nassau Island.^[12] Over the next few days the depression remained in the same general area before the final advisory was issued on February 15.^[12] On February 28, the FMS reported that two tropical depressions had developed within the basin.^[12] The first depression developed about 555 km (345 mi) to the northwest the French Polynesian island of Tahiti, before the final warning was issued during the next day after no development had occurred.^[12] The second depression developed about 500 km (310 mi) to the southeast of Honiara on the Solomon island of Guadalcanal, over the next couple of days the depression drifted towards the southeast, before the final warning was issued on March 2.^[75]

Season effects

This table lists all the storms that developed in the South Pacific basin during the 1997–98 season. It includes their intensity on the Australian Tropical cyclone intensity scale, duration, name, areas affected, deaths, and damages. For most storms the data is taken from RSMC Nadi's and or TCWC Wellington's archives, however data for 03P has been taken from the JTWC/NPMOC archives as opposed to RSMC Nadi's or TCWC Wellington's, and thus the winds are over 1-minute as opposed to 10-minutes.

Name	Dates	Peak intensity			Areas affected	Damage (USD)	Deaths	Refs
Name	Dates	Category	Wind speed	Pressure	Areas affected	Damage (USD)	Deaths	Refs
Lusi	October 8 - 12	Category 2 tropical cyclone	95 km/h (60 mph)	985 hPa (29.09 inHg)	Vanuatu, Fiji	None	None	^[17]
03P	October 26 – 28	Tropical Depression	55 km/h (35 mph)	997 hPa (29.44 inHg)	None	None	None	^[91]
Martin	October 27 – November 5	Category 3 severe tropical cyclone	155 km/h (100 mph)	945 hPa (27.91 inHg)	Cook Islands, French Polynesia	$17.6 million	28	^[8]^[93]^[94]
Nute	November 18 – 19	Category 2 tropical cyclone	110 km/h (70 mph)	975 hPa (28.79 inHg)	None	None	None	^[31]
Osea	November 22 – 28	Category 3 severe tropical cyclone	150 km/h (90 mph)	950 hPa (28.05 inHg)	French Polynesia		None
Pam	December 6 – 10	Category 2 tropical cyclone	110 km/h (70 mph)	975 hPa (28.79 inHg)	Cook Islands	Minor	None	^[8]
Susan	December 20 – January 9	Category 5 severe tropical cyclone	230 km/h (145 mph)	900 hPa (26.56 inHg)	Solomon Islands, Vanuatu, Fiji	$100,000	1	^[54]^[95]
Ron	January 1 – 8	Category 5 severe tropical cyclone	230 km/h (145 mph)	900 hPa (26.56 inHg)	Samoa, Wallis and Futuna, Tonga		None
Katrina	January 7 – 11	Category 3 severe tropical cyclone	150 km/h (90 mph)	955 hPa (28.20 inHg)	Solomon Islands, Vanuatu	$8.66 million	2	^[96]
Tui	January 25 – 27	Category 1 tropical cyclone	75 km/h (45 mph)	990 hPa (29.25 inHg)	Samoan islands	$1 million	1	^[96]
Ursula	January 29 – February 2	Category 2 tropical cyclone	110 km/h (70 mph)	975 hPa (28.79 inHg)	French Polynesia	Minor	None
Veli	January 30 – February 3	Category 2 tropical cyclone	100 km/h (65 mph)	985 hPa (29.09 inHg)	French Polynesia	Minor	None
Wes	January 31 – February 5	Category 2 tropical cyclone	95 km/h (60 mph)	985 hPa (29.09 inHg)	Cook Islands, French Polynesia	None	10
Unnamed	February 11 – 15	Tropical Depression	65 km/h (40 mph)	995 hPa, (29.39 inHg)	None	None	None	^[97]
Unnamed	February 28 – March 2	Tropical Depression	45 km/h (30 mph)	997 hPa, (29.44 inHg)	None	None	None	^[97]
Unnamed	February 28 – March 1	Tropical Depression	45 km/h (30 mph)	998 hPa, (29.47 inHg)	None	None	None	^[97]
Yali	March 18 – 25	Category 3 severe tropical cyclone	130 km/h (80 mph)	965 hPa (28.50 inHg)	Melanesia, Australia, New Zealand	$6 million	1	^[98]
Zuman	March 29 – April 5	Category 3 severe tropical cyclone	150 km/h (90 mph)	955 hPa (28.20 inHg)	Vanuatu, New Caledonia	$6 million	None	^[98]
Alan	April 17 – 26	Category 1 tropical cyclone	75 km/h (45 mph)	992 hPa (29.31 inHg)	French Polynesia		10	^[86]
Bart	April 28 – May 5	Category 1 tropical cyclone	85 km/h (50 mph)	987 hPa (29.15 inHg)	French Polynesia	Minor	10	^[8]^[90]
Season aggregates
20 systems	October 8 – May 5		230 km/h (145 mph)	900 hPa (26.56 inHg)			53

References

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^ ^a ^b Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center (December 17, 2002). "Tropical Cyclone 16P best track analysis". United States Navy, United States Air Force. Retrieved June 2, 2011.
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External links

[1997-98_BoM-1] ^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ ^j ^k ^l ^m ⁿ ^o ^p ^q ^r ^s ^t ^u ^v ^w Chappel Lori-Carmen; Bate Peter W (June 2, 2000). "The South Pacific and Southeast Indian Ocean Tropical Cyclone Season 1997–98" (PDF). Australian Meteorological Magazine. 49. Australian Bureau of Meteorology: 135–136. Archived from the original (PDF) on June 30, 2014. Retrieved July 1, 2014. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[2010-11_Prediction-2] Climate Services Division (October 26, 2010). Tropical Cyclone Guidance for Season 2010/11 for the Fiji and the Southwest Pacific (PDF) (Report). Fiji Meteorological Service. Archived from the original (PDF) on February 27, 2012. Retrieved April 6, 2012. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[2015-16_SO-3] RSMC Nadi — Tropical Cyclone Centre (October 22, 2015). "2015–16 Tropical Cyclone Season Outlook in the Regional Specialised Meteorological Centre Nadi – Tropical Cyclone Centre (RSMC Nadi – TCC) Area of Responsibility (AOR)" (PDF). Fiji Meteorological Service. Archived from the original (PDF) on October 22, 2015. Retrieved October 22, 2015. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[4] Samoa News — Pacific Islands report. (October 1, 1997). "Governor Tauese predicts Hurricane to hit American Samoa this year". Pacific Islands Development Program/Center for Pacific Islands Studies. Archived from the original on March 10, 2012. Retrieved February 22, 2012. {{cite news}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[5] Pacific Islands Report (October 9, 1997). "Cook Islands face possibility of worst cyclone season in years". Pacific Islands Development Program/Center for Pacific Islands Studies. Archived from the original on March 10, 2012. Retrieved July 26, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NIWA-6] National Institute of Water and Atmospheric Research (November 27, 1997). "El Niño predicted to cause more frequent tropical cyclones in South Pacific". National Oceanic and Atmospheric Administration. Archived from the original on March 10, 2012. Retrieved June 19, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[No_biggie's-7] "No big cyclones expected". The Evening Post. Wellington, New Zealand. December 17, 1997. p. 18. – via Lexis Nexis (subscription required)

[97-98_ATCR-8] ^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ ^j ^k ^l ^m ⁿ ^o ^p ^q ^r ^s ^t ^u ^v ^w ^x ^y ^z ^aa ^ab ^ac ^ad ^ae ^af ^ag ^ah ^ai ^aj ^ak ^al ^am ^an RSMC Nadi — Tropical Cyclone Centre (August 29, 2007). RSMC Nadi Tropical Cyclone Seasonal Summary 1997-98 (PDF) (Report). Fiji Meteorological Service. Archived from the original (PDF) on August 1, 2010. Retrieved May 29, 2011. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

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[GP_Nov-10] ^ ^a ^b ^c ^d ^e ^f ^g Padgett, Gary. Monthly Global Tropical Cyclone Summary November 1997 (Report). Archived from the original on November 25, 2012. Retrieved November 11, 2012. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[11] ttp://dailypost.vu/news/developing-el-nino-predicted-stronger-than---dubbed-godzilla/article_fe5cafeb-3ac9-5da5-b17d-9c3f29359515.html

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[SPAC_TCOP-13] RA V Tropical Cyclone Committee (May 5, 2015). Tropical Cyclone Operational Plan for the South-East Indian Ocean and the Southern Pacific Ocean 2014 (PDF) (Report). World Meteorological Organization. pp. 2B-1–2B-4 (23–26). Archived from the original (PDF) on May 24, 2015. Retrieved May 6, 2015. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[DTDSOCT97-14] Darwin Regional Specialised Meteorological Centre. "October 1997" (PDF). Darwin Tropical Diagnostic Statement. 16 (10). Australian: Bureau of Meteorology: 2–3. ISSN 1321-4233. Retrieved January 11, 2012.

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[19] Terry, James P (2007). Tropical cyclones: climatology and impacts in the South Pacific. Springer. ISBN 978-0-387-71542-1. Retrieved September 21, 2015.

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[NPMOC_Martin_BT-24] Naval Pacific Meteorology and Oceanography Center; Joint Typhoon Warning Center. Tropical Cyclone 04P (Martin) best track analysis (Report). United States Navy, United States Air Force. Retrieved July 23, 2013.

[NPMOC_AD_8-25] Naval Pacific Meteorology and Oceanography Center (November 3, 1997). Tropical Cyclone 04P (Martin) Warning 8 November 3, 1997 09z (Report). United States Navy, United States Air Force. Archived from the original on August 1, 2013. Retrieved August 1, 2013. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_AD_9-26] Naval Pacific Meteorology and Oceanography Center (November 3, 1997). Tropical Cyclone 04P (Martin) Warning 9 November 3, 1997 21z (Report). United States Navy, United States Air Force. Archived from the original on August 1, 2013. Retrieved August 1, 2013. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_AD_10-27] Naval Pacific Meteorology and Oceanography Center (November 4, 1997). Tropical Cyclone 04P (Martin) Warning 10 November 4, 1997 03z (Report). United States Navy, United States Air Force. Archived from the original on August 1, 2013. Retrieved August 1, 2013. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_AD_11-28] Naval Pacific Meteorology and Oceanography Center (November 4, 1997). Tropical Cyclone 04P (Martin) Warning 11 November 4, 1997 21z (Report). United States Navy, United States Air Force. Archived from the original on August 1, 2013. Retrieved August 1, 2013. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[05P_BT-29] Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center (2002). "Tropical Cyclone 05P (Nute) best track analysis". United States Navy, United States Air Force. Retrieved May 30, 2011.

[DTDSNOV97-30] Darwin Regional Specialised Meteorological Centre (1997). "November 1997" (PDF). Darwin Tropical Diagnostic Statement. 16 (11). Australian Bureau of Meteorology: 2. ISSN 1321-4233. Retrieved March 1, 2012.

[Nute_TCR-31] Brisbane Tropical Cyclone Warning Center (2010). "Tropical Cyclone Nute". Australian Bureau of Meteorology. Retrieved May 30, 2011.

[05P_AD-32] Joint Typhoon Warning Center (1997). "Tropical Cyclone 05P (Nute) Advisories". Australian Severe Weather. Archived from the original on July 6, 2012. Retrieved May 30, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[JTWC_Osea_BT-33] Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center. "Tropical Cyclone 06P (Osea) best track analysis". United States Navy, United States Air Force. Retrieved November 14, 2012.

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[NPMOC_4-35] Naval Pacific Meteorology and Oceanography Center. "Tropical Cyclone 06P (Osea) Warning 4 November 25, 1997 03z". United States Navy, United States Air Force. Archived from the original on November 25, 2012. Retrieved November 25, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_8-36] Naval Pacific Meteorology and Oceanography Center. "Tropical Cyclone 06P (Osea) Warning 8, November 27, 1997, 00z". United States Navy, United States Air Force. Archived from the original on November 24, 2012. Retrieved November 24, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[GP-37] Padgett, Gary. Monthly Global Tropical Cyclone Summary November 1997 (Report). Archived from the original on November 25, 2012. Retrieved November 11, 2012. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[elninohavoc-38] "Powerful El Nino Causing Havoc in Pacific". Papeete, Tahiti: International Indigenous ICT Task Force. February 24, 2010. Retrieved November 25, 2012.

[FP1-39] The Ensign of the Church of Jesus Christ of Latter-Day Saints, Volume 28. The Church. 1998.

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[drylanhorticulture-45] Cauchois, Mickaelle-Hinanui; Service du Patrimoine, Ministere de la Culture (2002). "Dryland Horticulture in Maupiti: An Ethnoarchaeological Study" (PDF). University of Hawai'i Press. p. 277. Retrieved November 25, 2012.

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[47] Joint Typhoon Warning Center. "Tropical Cyclone 07P Warning 1 December 6, 1997 21z". United States Navy, United States Air Force. Archived from the original on February 23, 2014. Retrieved February 23, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[07P_BT-48] Joint Typhoon Warning Center. "Tropical Cyclone 07P (Pam) best track analysis". United States Navy, United States Air Force. Retrieved February 23, 2014.

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[57] Naval Pacific Meteorological and Oceanographic Center (January 9, 1998). "Tropical Cyclone 11P (Susan) Warning 13 January 9, 1998 0300z". United States Navy, United States Air Force. Archived from the original on January 6, 2012. Retrieved July 18, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[58] "Blame Cyclone Susan for cold snap". The Southland Times. New Zealand: The Southland Times Co. Ltd. January 10, 1998. p. 1.

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[60] "Cyclone Tui heading toward Samoa". Agence France Presse. January 25, 1998.

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[62] National Climatic Data Center. Del Greco, Stephen; Hinson, Stuart (eds.). "January 1998" (PDF). Storm Data. 39 (1). National Environmental Satellite Data, And Information Service, National Oceanic And Atmospheric Administration: 15. Archived from the original (PDF) on August 9, 2012. Retrieved August 9, 2012. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[17P-63] Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center (December 17, 2002). "Tropical Cyclone 17P best track analysis". United States Navy, United States Air Force. Retrieved June 5, 2011.

[GP_March_1998-64] ^ ^a ^b ^c ^d ^e ^f ^g ^h Padgett, Gary (1998). "Monthly Global Tropical Cyclone Summary March 1998". Australian Severe Weather. Archived from the original on November 28, 2015. Retrieved November 28, 2015. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[VW1-65] "Tropical Cyclone 18P (Veli) warning February 1, 1998 09z". Naval Pacific Meteorology and Oceanography Center. February 1, 1998. Archived from the original on July 30, 2012. Retrieved August 5, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[18P_BT-66] "Tropical Cyclone 18P (Katrina) best track analysis". Naval Pacific Meteorology and Oceanography Center. Archived from the original on August 5, 2012. Retrieved August 4, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[VW6-67] Naval Pacific Meteorology and Oceanography Center (February 1, 1998). "Tropical Cyclone 18P (Veli) warning February 3, 1998 21z". United States Navy, United States Air Force. Archived from the original on August 4, 2012. Retrieved August 5, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[68] Naval Pacific Meteorology and Oceanography Center (February 1, 1998). Tropical Cyclone 19P (Wes) Warning 1 February 1, 1998 15z (Report). United States Navy, United States Air Force. Archived from the original on December 28, 2013. Retrieved June 28, 2014. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[69] Naval Pacific Meteorology and Oceanography Center (February 3, 1998). Tropical Cyclone 19P (Wes) Warning 5 February 3, 1998 15z (Report). United States Navy, United States Air Force. Archived from the original on June 29, 2014. Retrieved June 29, 2014. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[70] Naval Pacific Meteorology and Oceanography Center (February 4, 1998). Tropical Cyclone 19P (Wes) Warning 6 February 4, 1998 03z (Report). United States Navy, United States Air Force. Archived from the original on June 29, 2014. Retrieved June 29, 2014. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Landslide_10-71] "Six still missing after landslide kills ten on island". Australian Associated Press. February 8, 1998. – via Lexis Nexis (subscription required)

[Landslide_2-72] "Landslide on Tahaa, French Polynesia kills at least 10". Radio Australia. February 8, 1998. Archived from the original on June 28, 2014. {{cite news}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[29P_BT-73] Joint Typhoon Warning Center. "Tropical Cyclone 29P (Yali) best track analysis". United States Navy, United States Air Force. Retrieved February 15, 2014.

[TCFA_Y-74] Joint Typhoon Warning Center. "Tropical Cyclone Formation Alert March 17, 1998 23z". United States Navy, United States Air Force. Archived from the original on February 15, 2014. Retrieved February 15, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Mar_98-75] ^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ ^j ^k ^l ^m Padgett, Gary (1998). "Monthly Global Tropical Cyclone Summary March 1998". Archived from the original on June 5, 2011. Retrieved June 27, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[JTWC_1-76] Joint Typhoon Warning Center. "Tropical Cyclone 29P Warning 3 March 19, 1998 21z". United States Navy, United States Air Force. Archived from the original on February 15, 2014. Retrieved February 15, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[DTDSAPR98-77] Darwin Regional Specialised Meteorological Centre. "April 1998" (PDF). Darwin Tropical Diagnostic Statement. 17 (4). Australian Bureau of Meteorology: 2. ISSN 1321-4233. Retrieved February 25, 2014.

[78] "Tropical Cyclone 29P (Zuman) warning March 30, 1998 03z". Joint Typhoon Warning Center. March 30, 1998. Retrieved November 21, 2015.

[GP_9804-79] ^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ ^j Padgett, Gary (1998). "Monthly Global Tropical Cyclone Summary April 1998". Archived from the original on January 15, 2012. Retrieved May 29, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[April_tracks-80] Padgett, Gary. "Monthly Global Tropical Cyclone Tracks April 1998". Archived from the original on February 8, 2014. Retrieved February 8, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_A1-81] Naval Pacific Meteorology and Oceanography Center. "Tropical Cyclone 32P (Alan) Warning 1 April 22, 1998 21z". United States Navy, United States Air Force. Archived from the original on February 8, 2014. Retrieved February 8, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_3-82] Naval Pacific Meteorology and Oceanography Center. "Tropical Cyclone 32P (Alan) Warning 3 April 23, 1998 21z". United States Navy, United States Air Force. Archived from the original on February 9, 2014. Retrieved February 9, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[NPMOC_7-83] Naval Pacific Meteorology and Oceanography Center (April 26, 1998). "Tropical Cyclone 32P (Alan) Warning 7 April 26, 1998 03z". United States Navy, United States Air Force. Archived from the original on February 9, 2014. Retrieved February 9, 2014. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Eight_dead-84] "At least eight killed by French Polynesia cyclone". Pacific Islands Report. Pacific Islands Development Program/Center for Pacific Islands Studies. April 27, 1998. Archived from the original on February 9, 2014. Retrieved February 9, 2014. {{cite news}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[GP_9805-85] Padgett, Gary (1998). "Monthly Global Tropical Cyclone Summary May 1998". Archived from the original on February 9, 2014. Retrieved May 29, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[pidp.org-86] "French Polynesia cyclone deaths rise to 10". Pacific Islands Report. Pacific Islands Development Program/Center for Pacific Islands Studies. May 1, 1998. Archived from the original on February 9, 2014. Retrieved February 9, 2014. {{cite news}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[37P_BT-87] Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center (December 17, 2002). "Tropical Cyclone 37P (Bart) best track analysis". United States Navy, United States Air Force. Retrieved May 29, 2011.

[Bart1-88] Naval Pacific Meteorology and Oceanography Center (April 30, 1998). "Tropical Cyclone 37P (Bart) warning April 30, 1998 18z". United States Navy, United States Air Force. Archived from the original on June 5, 2011. Retrieved June 5, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Bart3-89] Naval Pacific Meteorology and Oceanography Center (April 30, 1998). "Tropical Cyclone 37P (Bart) warning May 2, 1998 06z". United States Navy, United States Air Force. Archived from the original on January 14, 2012. Retrieved June 5, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[PDN:Bart-90] May, Jutta (September 17, 2008). "Event Information: Tropical Cyclone Bart". Pacific Disaster.Net. Archived from the original on January 15, 2012. Retrieved June 2, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[03P-91] Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center (December 17, 2002). "Tropical Cyclone 03P best track analysis". United States Navy, United States Air Force. Retrieved June 5, 2011.

[03P_W1-92] Joint Typhoon Warning Center (October 26, 1997). "Tropical Cyclone 03P Warning 1 October 26, 1997 1500 UTC". United States Navy, United States Air Force. Archived from the original on January 15, 2012. Retrieved June 30, 2011. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[PCR:Martin-93] Asian Development Bank (November 29, 2000). Project completion report on the cyclone emergency rehabilitation project (Loan 1588-COOSF) in the Cook Islands (PDF) (Report). p. 8. Retrieved January 17, 2012.

[94] Cook Islands Government (June 20, 2007). "Coroner confirms Cyclone Martin Victims". Archived from the original on August 1, 2010. Retrieved April 30, 2010. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Sol-95] "Tropical Cyclones/Depressions that passed through Solomon Islands Region" (PDF). Solomon Islands Meteorological Service. September 13, 2009. Archived from the original (PDF) on March 9, 2013. Retrieved November 25, 2015. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[Impact-96] McKenzie, Emily; Prasad, Biman; Kaloumaira, Atu (2005). Economic Impact of Natural Disasters on development in the Pacific Volume 1: Research Report (PDF) (Report). pp. 10–89. Archived from the original (PDF) on February 25, 2010. Retrieved June 29, 2010. {{cite report}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[feb_tracks-97] Padgett, Gary. "Monthly Global Tropical Cyclone Tracks February 1998". Archived from the original on July 24, 2012. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[WMO_Assessment-98] Report of the WMO Post-Tropical Cyclone "Pam" Expert Mission to Vanuatu (PDF) (Report). World Meteorological Organization. p. 22.

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@@ Line 35: / Line 35: @@
 ! Record !! <small>[[Tropical Cyclone|Tropical<br>Cyclone]]</small> !! <small>[[Severe Tropical Cyclone|Severe Tropical<br>Cyclone]]</small> !! <small><br>Ref</small>
 |-
-| Average activity: <small>(1969–70&nbsp;– 1996–97)</Small> || align=right|7&nbsp;– 8 || align=right|4 ||<ref name="1997-98 BoM">{{cite journal|publisher=Australian Bureau of Meteorology |title=The South Pacific and Southeast Indian Ocean Tropical Cyclone Season 1997–98 |url=http://www.bom.gov.au/amm/docs/2000/chappel.pdf |accessdate=July 1, 2014 |pages=135–136 |deadurl=no |journal=Australian Meteorological Magazine |author1=Chappel Lori-Carmen |date=June 2, 2000 |author2=Bate Peter W |archiveurl=http://www.webcitation.org/6Qhrcv0LG?url=http%3A%2F%2Fwww.bom.gov.au%2Famm%2Fdocs%2F2000%2Fchappel.pdf |archivedate=June 30, 2014 |volume=49 |df=mdy }}</ref>
+| Average activity: <small>(1969–70&nbsp;– 1996–97)</Small> || align=right|7&nbsp;– 8 || align=right|4 ||<ref name="1997-98 BoM">{{cite journal|publisher=Australian Bureau of Meteorology |title=The South Pacific and Southeast Indian Ocean Tropical Cyclone Season 1997–98 |url=http://www.bom.gov.au/amm/docs/2000/chappel.pdf |accessdate=July 1, 2014 |pages=135–136 |deadurl=no |journal=Australian Meteorological Magazine |author1=Chappel Lori-Carmen |date=June 2, 2000 |author2=Bate Peter W |archiveurl=http://www.webcitation.org/6Qhrcv0LG?url=http://www.bom.gov.au/amm/docs/2000/chappel.pdf |archivedate=June 30, 2014 |volume=49 |df=mdy }}</ref>
 |-
-| ''Record high activity:'' || align="right"|[[1982–83 South Pacific cyclone season|1982-83]]: 14 || align="right"|[[1982–83 South Pacific cyclone season|1982–83]]:10 ||<ref name="2010-11 Prediction">{{cite report|publisher=Fiji Meteorological Service |title=Tropical Cyclone Guidance for Season 2010/11 for the Fiji and the Southwest Pacific |url=http://www.met.gov.fj/2010_2011%20TC%20Guide.pdf |date=October 26, 2010 |archiveurl=http://www.webcitation.org/65kvh9FwY?url=http%3A%2F%2Fwww.met.gov.fj%2F2010_2011%2520TC%2520Guide.pdf |author=Climate Services Division |accessdate=April 6, 2012 |archivedate=February 27, 2012 |deadurl=no |df=mdy }}</ref>
+| ''Record high activity:'' || align="right"|[[1982–83 South Pacific cyclone season|1982-83]]: 14 || align="right"|[[1982–83 South Pacific cyclone season|1982–83]]:10 ||<ref name="2010-11 Prediction">{{cite report|publisher=Fiji Meteorological Service |title=Tropical Cyclone Guidance for Season 2010/11 for the Fiji and the Southwest Pacific |url=http://www.met.gov.fj/2010_2011%20TC%20Guide.pdf |date=October 26, 2010 |archiveurl=http://www.webcitation.org/65kvh9FwY?url=http://www.met.gov.fj/2010_2011%20TC%20Guide.pdf |author=Climate Services Division |accessdate=April 6, 2012 |archivedate=February 27, 2012 |deadurl=yes |df=mdy }}</ref>
 |-
 | ''Record low activity'' || align=right|[[1994–95 South Pacific cyclone season|1994–95]]: 3 || align=right|[[1994–95 South Pacific cyclone season|1994–95]]:&nbsp;0 ||<ref name="2010-11 Prediction"/>
 |-
-| ''Activity during this season:'' || align=right|16 || align=right|7 ||<ref name="2015-16 SO">{{cite web|title=2015–16 Tropical Cyclone Season Outlook in the Regional Specialised Meteorological Centre Nadi&nbsp;– Tropical Cyclone Centre (RSMC Nadi&nbsp;– TCC) Area of Responsibility (AOR) |accessdate=October 22, 2015 |date=October 22, 2015 |author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |publisher=Fiji Meteorological Service |url=http://www.met.gov.fj/aifs_prods/Tropical_Cyclone_Guidance_2015_16.pdf |archiveurl=http://www.webcitation.org/6cTPF9dra?url=http%3A%2F%2Fwww.met.gov.fj%2Faifs_prods%2FTropical_Cyclone_Guidance_2015_16.pdf |archivedate=October 22, 2015 |deadurl=no |df=mdy }}</ref>
+| ''Activity during this season:'' || align=right|16 || align=right|7 ||<ref name="2015-16 SO">{{cite web|title=2015–16 Tropical Cyclone Season Outlook in the Regional Specialised Meteorological Centre Nadi&nbsp;– Tropical Cyclone Centre (RSMC Nadi&nbsp;– TCC) Area of Responsibility (AOR) |accessdate=October 22, 2015 |date=October 22, 2015 |author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |publisher=Fiji Meteorological Service |url=http://www.met.gov.fj/aifs_prods/Tropical_Cyclone_Guidance_2015_16.pdf |archiveurl=http://www.webcitation.org/6cTPF9dra?url=http://www.met.gov.fj/aifs_prods/Tropical_Cyclone_Guidance_2015_16.pdf |archivedate=October 22, 2015 |deadurl=no |df=mdy }}</ref>
 |}
-Ahead of the season officially starting on November 1, the American Samoan Governor reported that traditionalists were forecasting a hurricane to affect [[American Samoa]], during the season after the big breadfruit and mango harvest that the island nation had experienced.<ref>{{cite news|url=http://archives.pireport.org/archive/1997/october/10-02-10.html |title=Governor Tauese predicts Hurricane to hit American Samoa this year |date=October 1, 1997 |author=Samoa News&nbsp;— Pacific Islands report. |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 22, 2012 |archiveurl=http://www.webcitation.org/663jfd5KG?url=http%3A%2F%2Farchives.pireport.org%2Farchive%2F1997%2Foctober%2F10-02-10.html |archivedate=March 10, 2012 |deadurl=no |df=mdy }}</ref> The Cook Islands Meteorological Service and National Disasters Committee warned islanders that they could expect the "worst cyclone season in years."<ref>{{cite web|url=http://archives.pireport.org/archive/1997/october/10-09-02.html |title=Cook Islands face possibility of worst cyclone season in years |date=October 9, 1997 |deadurl=no |author=Pacific Islands Report |accessdate=July 26, 2011 |archiveurl=http://www.webcitation.org/663jaemUj?url=http%3A%2F%2Farchives.pireport.org%2Farchive%2F1997%2Foctober%2F10-09-02.html |archivedate=March 10, 2012 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |df=mdy }}</ref> On November 27, New Zealand's [[National Institute of Water and Atmospheric Research]], issued a press release, which predicted that because of the strong [[El Niño|El Niño phenomenon]], there would be more tropical cyclones than average.<ref name="NIWA">{{cite web|title=El Niño predicted to cause more frequent tropical cyclones in South Pacific |date=November 27, 1997 |author=National Institute of Water and Atmospheric Research |url=http://www.soest.hawaii.edu/MET/Enso/peu/update.dir/NIWA-TCPR.html |publisher=National Oceanic and Atmospheric Administration |accessdate=June 19, 2011 |archiveurl=http://www.webcitation.org/663jrXQxz?url=http%3A%2F%2Fwww.ideademo.org%2FMET%2FEnso%2Fpeu%2Fupdate.dir%2FNIWA-TCPR.html |archivedate=March 10, 2012 |deadurl=no |df=mdy }}</ref> In particular they predicted that due to the strong El Niño, countries within the western part of the basin were likely to see fewer tropical cyclones during the season than countries within the eastern part of the basin.<ref name="NIWA"/>
+Ahead of the season officially starting on November 1, the American Samoan Governor reported that traditionalists were forecasting a hurricane to affect [[American Samoa]], during the season after the big breadfruit and mango harvest that the island nation had experienced.<ref>{{cite news|url=http://archives.pireport.org/archive/1997/october/10-02-10.html |title=Governor Tauese predicts Hurricane to hit American Samoa this year |date=October 1, 1997 |author=Samoa News&nbsp;— Pacific Islands report. |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 22, 2012 |archiveurl=http://www.webcitation.org/663jfd5KG?url=http://archives.pireport.org/archive/1997/october/10-02-10.html |archivedate=March 10, 2012 |deadurl=no |df=mdy }}</ref> The Cook Islands Meteorological Service and National Disasters Committee warned islanders that they could expect the "worst cyclone season in years."<ref>{{cite web|url=http://archives.pireport.org/archive/1997/october/10-09-02.html |title=Cook Islands face possibility of worst cyclone season in years |date=October 9, 1997 |deadurl=no |author=Pacific Islands Report |accessdate=July 26, 2011 |archiveurl=http://www.webcitation.org/663jaemUj?url=http://archives.pireport.org/archive/1997/october/10-09-02.html |archivedate=March 10, 2012 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |df=mdy }}</ref> On November 27, New Zealand's [[National Institute of Water and Atmospheric Research]], issued a press release, which predicted that because of the strong [[El Niño|El Niño phenomenon]], there would be more tropical cyclones than average.<ref name="NIWA">{{cite web|title=El Niño predicted to cause more frequent tropical cyclones in South Pacific |date=November 27, 1997 |author=National Institute of Water and Atmospheric Research |url=http://www.soest.hawaii.edu/MET/Enso/peu/update.dir/NIWA-TCPR.html |publisher=National Oceanic and Atmospheric Administration |accessdate=June 19, 2011 |archiveurl=http://www.webcitation.org/663jrXQxz?url=http://www.ideademo.org/MET/Enso/peu/update.dir/NIWA-TCPR.html |archivedate=March 10, 2012 |deadurl=no |df=mdy }}</ref> In particular they predicted that due to the strong El Niño, countries within the western part of the basin were likely to see fewer tropical cyclones during the season than countries within the eastern part of the basin.<ref name="NIWA"/>
 The Southern [[Cook Islands]], [[Tonga]], [[Tuvalu]] and [[French Polynesia]], were predicted to have an increased risk, while [[Fiji]] was forecast to have an average risk of being affected by a tropical cyclone.<ref name="NIWA"/> NIWA also reported that Cyclone Martin's impact on the Northern Cook Islands was an early sign of what could be expected during the season, because the system had occurred further east than normal.<ref name="NIWA"/> In mid December the Cook Islands Meteorological Service director commented to the media that from now on, by the time cyclones reached Raro-Tonga would have lost their intensity, while a spokesperson for NIWA commented that holidaymakers heading for the Pacific had a little chance of running into a cyclone as the damaging core of the cyclone was expected to be over the ocean while some cyclones were expected to be relatively weak.<ref name="No biggie's">{{cite news|title=No big cyclones expected|newspaper=The Evening Post|date=December 17, 1997|location=Wellington, New Zealand|page=18}} {{subscription required|via=Lexis Nexis}}</ref> It was also noted that collectively the Pacific Islands Meteorological Services were bracing for up to 15 tropical cyclones during the season, compared to 12 during an average season.<ref name="No biggie's"/>
@@ Line 120: / Line 120: @@
 </center>
-The 1997–98 season was one of the most active and longest [[South Pacific tropical cyclone season]]s on record, with 16&nbsp;[[tropical cyclones]] occurring within the [[Tropical cyclone basin#South Pacific|South Pacific basin]] between [[160th meridian east|160°E]] and [[120th meridian west|120°W]].<ref name="97-98 ATCR">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |publisher=Fiji Meteorological Service |title=RSMC Nadi Tropical Cyclone Seasonal Summary 1997-98 |date=August 29, 2007 |archivedate=August 1, 2010 |accessdate=May 29, 2011 |url=http://www.pacificdisaster.net/pdnadmin/data/original/TC_Seasonal_Summary_97-98.pdf |archiveurl=http://www.webcitation.org/5rfDHEnbo?url=http%3A%2F%2Fwww.met.gov.fj%2Fdocuments%2FTC_Seasonal_Summary_97-981190690538.pdf |deadurl=no |df=mdy }}</ref> The season was characterised by a very strong [[1997–98 El Niño Event|El Niño Event]], which caused the [[South Pacific Convergence Zone]], to move from its usual position near the Solomon Islands to the Northern Cook Islands.<ref name="1997-98 BoM"/> As a result, ten tropical cyclones formed to the east of the International Dateline, with seven of these tropical cyclones going on to affect French Polynesia.<ref name="1997-98 BoM"/> After the 1996-97 season had one of the latest ends to a season on record, the 1997-98 season started early with three tropical systems observed before the start of the season on November 1, 1997.<ref name="97-98 ATCR"/> Two other tropical systems, including the precursor tropical disturbance to Severe Tropical Cyclone Martin developed, before the official start of the season on November 1, 1997.<ref name="GP1097"/> Severe Tropical Cyclone Martin impacted the Cook Islands and French Polynesia, where it caused significant damage and 28 deaths during the opening days of the season.<ref name="GP1097"/> Tropical Cyclone Nute was named on November 18, before it moved out of the basin as a Category 2 tropical cyclone during November 19.<ref name="GP Nov"/> During the rest of November, several tropical disturbances developed along the South Pacific Convergence Zone, including the precursor system to Severe Tropical Cyclone Osea and Tropical Cyclone Pam.<ref name="GP Nov"/><ref>http://dailypost.vu/news/developing-el-nino-predicted-stronger-than---dubbed-godzilla/article_fe5cafeb-3ac9-5da5-b17d-9c3f29359515.html</ref> Osea was named
+The 1997–98 season was one of the most active and longest [[South Pacific tropical cyclone season]]s on record, with 16&nbsp;[[tropical cyclones]] occurring within the [[Tropical cyclone basin#South Pacific|South Pacific basin]] between [[160th meridian east|160°E]] and [[120th meridian west|120°W]].<ref name="97-98 ATCR">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |publisher=Fiji Meteorological Service |title=RSMC Nadi Tropical Cyclone Seasonal Summary 1997-98 |date=August 29, 2007 |archivedate=August 1, 2010 |accessdate=May 29, 2011 |url=http://www.pacificdisaster.net/pdnadmin/data/original/TC_Seasonal_Summary_97-98.pdf |archiveurl=http://www.webcitation.org/5rfDHEnbo?url=http://www.met.gov.fj/documents/TC_Seasonal_Summary_97-981190690538.pdf |deadurl=no |df=mdy }}</ref> The season was characterised by a very strong [[1997–98 El Niño Event|El Niño Event]], which caused the [[South Pacific Convergence Zone]], to move from its usual position near the Solomon Islands to the Northern Cook Islands.<ref name="1997-98 BoM"/> As a result, ten tropical cyclones formed to the east of the International Dateline, with seven of these tropical cyclones going on to affect French Polynesia.<ref name="1997-98 BoM"/> After the 1996-97 season had one of the latest ends to a season on record, the 1997-98 season started early with three tropical systems observed before the start of the season on November 1, 1997.<ref name="97-98 ATCR"/> Two other tropical systems, including the precursor tropical disturbance to Severe Tropical Cyclone Martin developed, before the official start of the season on November 1, 1997.<ref name="GP1097"/> Severe Tropical Cyclone Martin impacted the Cook Islands and French Polynesia, where it caused significant damage and 28 deaths during the opening days of the season.<ref name="GP1097"/> Tropical Cyclone Nute was named on November 18, before it moved out of the basin as a Category 2 tropical cyclone during November 19.<ref name="GP Nov"/> During the rest of November, several tropical disturbances developed along the South Pacific Convergence Zone, including the precursor system to Severe Tropical Cyclone Osea and Tropical Cyclone Pam.<ref name="GP Nov"/><ref>http://dailypost.vu/news/developing-el-nino-predicted-stronger-than---dubbed-godzilla/article_fe5cafeb-3ac9-5da5-b17d-9c3f29359515.html</ref> Osea was named
 Severe Tropical Cyclones Ron and Susan were both the strongest tropical cyclones of the season and were thought to be the strongest tropical cyclones in the region since [[Cyclone Hina (1985)|Severe Tropical Cyclone Hina]] of the [[1984–85 South Pacific cyclone season|1984-85 season]].<ref name="1997-98 BoM"/>
-After the final warnings on Cyclone Tui were issued a weak circulation remained in the vicinity of Samoa for several days, before a westerly surge from the monsoon resulted in a tropical cyclone developing during February 1.<ref name="1997-98 BoM"/> However, due to uncertainties in the continuation of Tui after several other weak low pressure areas had formed, RSMC Nadi decided to treat the cyclone as a separate system and named it Wes.<ref name="Feb 98">{{cite web|title=Monthly Global Tropical Cyclone Summary February 1998 |author=Padgett, Gary |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9802.htm |accessdate=February 22, 2014 |archiveurl=http://www.webcitation.org/6NZ59OgTb?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9802.htm |archivedate=February 22, 2014 |deadurl=no |df=mdy }}</ref>
+After the final warnings on Cyclone Tui were issued a weak circulation remained in the vicinity of Samoa for several days, before a westerly surge from the monsoon resulted in a tropical cyclone developing during February 1.<ref name="1997-98 BoM"/> However, due to uncertainties in the continuation of Tui after several other weak low pressure areas had formed, RSMC Nadi decided to treat the cyclone as a separate system and named it Wes.<ref name="Feb 98">{{cite web|title=Monthly Global Tropical Cyclone Summary February 1998 |author=Padgett, Gary |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9802.htm |accessdate=February 22, 2014 |archiveurl=http://www.webcitation.org/6NZ59OgTb?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9802.htm |archivedate=February 22, 2014 |deadurl=no |df=mdy }}</ref>
-Tropical Cyclone Bart developed during the final days of the season and caused ten deaths and minor damage to French Polynesia, before it dissipated during May 3. The names Katrina, Martin, Nute, Osea, Ron, Susan, Tui, Ursula and Veli, were subsequently retired from the lists of names for the region.<ref name="SPAC TCOP">{{cite report|author=RA V Tropical Cyclone Committee |publisher=World Meteorological Organization |title=Tropical Cyclone Operational Plan for the South-East Indian Ocean and the Southern Pacific Ocean 2014 |date=May 5, 2015 |pages=2B-1–2B-4 (23–26) |format=PDF |url=https://www.wmo.int/pages/prog/www/tcp/documents/TCP24_RAVOpPlan_2014_final.pdf |accessdate=May 6, 2015 |archiveurl=http://www.webcitation.org/6YlsJ3Q48?url=https%3A%2F%2Fwww.wmo.int%2Fpages%2Fprog%2Fwww%2Ftcp%2Fdocuments%2FTCP24_RAVOpPlan_2014_final.pdf |archivedate=May 24, 2015 |deadurl=no |df=mdy }}</ref>
+Tropical Cyclone Bart developed during the final days of the season and caused ten deaths and minor damage to French Polynesia, before it dissipated during May 3. The names Katrina, Martin, Nute, Osea, Ron, Susan, Tui, Ursula and Veli, were subsequently retired from the lists of names for the region.<ref name="SPAC TCOP">{{cite report|author=RA V Tropical Cyclone Committee |publisher=World Meteorological Organization |title=Tropical Cyclone Operational Plan for the South-East Indian Ocean and the Southern Pacific Ocean 2014 |date=May 5, 2015 |pages=2B-1–2B-4 (23–26) |format=PDF |url=https://www.wmo.int/pages/prog/www/tcp/documents/TCP24_RAVOpPlan_2014_final.pdf |accessdate=May 6, 2015 |archiveurl=http://www.webcitation.org/6YlsJ3Q48?url=https://www.wmo.int/pages/prog/www/tcp/documents/TCP24_RAVOpPlan_2014_final.pdf |archivedate=May 24, 2015 |deadurl=no |df=mdy }}</ref>
 {{Clear}}
@@ Line 145: / Line 145: @@
 {{See also|List of off-season South Pacific tropical cyclones}}
 On October 4, a cyclonic circulation became evident within an area of convection, that was located about 500&nbsp;km (310&nbsp;mi) to the southeast of [[Yaren District|Yaren]] in [[Nauru]].<ref name="DTDSOCT97">{{cite journal|title=October 1997|journal=Darwin Tropical Diagnostic Statement|publisher=Bureau of Meteorology|location=Australian|volume=16|issue=10|author=Darwin Regional Specialised Meteorological Centre|pages=2–3|issn=1321-4233|url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199710.pdf|accessdate=January 11, 2012}}</ref><ref name="02P BT">{{cite web|publisher=United States Navy, United States Air Force|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh021998.txt|title=Tropical Cyclone 02P (Lusi) best track analysis|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|accessdate=May 30, 2011|year=2002}}</ref> Over the next few days the system moved southwards, towards the upper subtropical ridge while outflow gradually developed further.<ref name="DTDSOCT97"/><ref name="02P BT"/> During October 8, the system was classified as a tropical depression as the system rapidly developed further, before the JTWC initiated
-initiated advisories on the depression and designated it as Tropical Cyclone 02P.<ref name="GP1097"/><ref name="W1">{{cite web|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 02P (Lusi) warning October 8, 1997 20z|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh021998.97100818.wrn|date=October 8, 1997|accessdate=June 29, 2011|author=Joint Typhoon Warning Center}}</ref><ref name="Lusi PR">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |title=Report on Tropical Cyclone Lusi October 6-12, 1997 |year=1997 |archivedate=February 27, 2014 |accessdate=February 27, 2014 |url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_FJI_FMS_TC_Lusi_1997_Prelimary_report.pdf |archiveurl=http://www.webcitation.org/6Ni7KwjhY?url=http%3A%2F%2Fwww.pacificdisaster.net%2Fpdnadmin%2Fdata%2Foriginal%2FCRP_FJI_FMS_TC_Lusi_1997_Prelimary_report.pdf |publisher=Fiji Meteorological Service |deadurl=no |df=mdy }}</ref> The FMS subsequently named the depression Lusi during the next day, as the system had intensified into the earliest tropical cyclone since 1970, while located about {{convert|1020|km|mi|disp=5|abbr=on}} to the northwest of Port Villa, Vanuatu.<ref name="GP1097"/><ref name="97-98 BT">{{cite web|date=May 22, 2009|title=RSMC Nadi&nbsp;— Tropical Cyclone Centre Best Track Data for 1997/98 Cyclone Season|publisher=International Best Track Archive for Climate Stewardship|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre|author3=TCWC Wellington|location=United States|work=Fiji Meteorological Service, Meteorological Service of New Zealand Limited, Australian Bureau of Meteorology|url=ftp://eclipse.ncdc.noaa.gov/pub/ibtracs/original-bt-data-files/nadi/RSMC%20Nadi%209798%20BT%20Data.txt.txt|accessdate=January 31, 2013|author2=TCWC Brisbane}}</ref><ref>{{cite book|author=Terry, James P|publisher=Springer|accessdate=September 21, 2015|year=2007|title=Tropical cyclones: climatology and impacts in the South Pacific|isbn=978-0-387-71542-1|url={{Google books|CUh3FXQFiDMC|page=49|plainurl=yes}}}}</ref> Over the next few days, Lusi moved towards the south-southeast, taking a so-called "gentleman's track" between Vanuatu and Fiji.<ref name="97-98 ATCR"/>
+initiated advisories on the depression and designated it as Tropical Cyclone 02P.<ref name="GP1097"/><ref name="W1">{{cite web|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 02P (Lusi) warning October 8, 1997 20z|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh021998.97100818.wrn|date=October 8, 1997|accessdate=June 29, 2011|author=Joint Typhoon Warning Center}}</ref><ref name="Lusi PR">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |title=Report on Tropical Cyclone Lusi October 6-12, 1997 |year=1997 |archivedate=February 27, 2014 |accessdate=February 27, 2014 |url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_FJI_FMS_TC_Lusi_1997_Prelimary_report.pdf |archiveurl=http://www.webcitation.org/6Ni7KwjhY?url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_FJI_FMS_TC_Lusi_1997_Prelimary_report.pdf |publisher=Fiji Meteorological Service |deadurl=no |df=mdy }}</ref> The FMS subsequently named the depression Lusi during the next day, as the system had intensified into the earliest tropical cyclone since 1970, while located about {{convert|1020|km|mi|disp=5|abbr=on}} to the northwest of Port Villa, Vanuatu.<ref name="GP1097"/><ref name="97-98 BT">{{cite web|date=May 22, 2009|title=RSMC Nadi&nbsp;— Tropical Cyclone Centre Best Track Data for 1997/98 Cyclone Season|publisher=International Best Track Archive for Climate Stewardship|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre|author3=TCWC Wellington|location=United States|work=Fiji Meteorological Service, Meteorological Service of New Zealand Limited, Australian Bureau of Meteorology|url=ftp://eclipse.ncdc.noaa.gov/pub/ibtracs/original-bt-data-files/nadi/RSMC%20Nadi%209798%20BT%20Data.txt.txt|accessdate=January 31, 2013|author2=TCWC Brisbane}}</ref><ref>{{cite book|author=Terry, James P|publisher=Springer|accessdate=September 21, 2015|year=2007|title=Tropical cyclones: climatology and impacts in the South Pacific|isbn=978-0-387-71542-1|url={{Google books|CUh3FXQFiDMC|page=49|plainurl=yes}}}}</ref> Over the next few days, Lusi moved towards the south-southeast, taking a so-called "gentleman's track" between Vanuatu and Fiji.<ref name="97-98 ATCR"/>
 During October 10, the JTWC reported that Lusi had peaked with 1-minute sustained wind speeds of 110&nbsp;km/h (70&nbsp;mph), while the system was located about {{convert|570|km|mi|disp=5|abbr=on}} to the northwest of Port Vila, Vanuatu.<ref name="02P BT"/> The FMS subsequently followed suit during the next day and estimated peak 10-minute sustained wind speeds of 100&nbsp;km/h (65&nbsp;mph).<ref name="97-98 BT"/> After it had peaked in intensity Lusi started to weaken in an area of cooler sea surface temperatures, while vertical windshear increased because of a mid level trough and strong north-westerlies.<ref name="97-98 ATCR"/><ref name="DTDSOCT97"/> During October 12, Lusi degenerated into an extratropical cyclone, before the remnants were last noted to the northeast of New Zealand<ref name="GP1097"/><ref name="02P BT"/>{{TCWC Wellington BT}} There was no impact caused by Lusi on any island, however, widespread heavy rainfall and gale force wind speeds were reported on several Fijian Islands.<ref name="Lusi PR"/>
@@ Line 163: / Line 163: @@
 }}
 {{main article|Cyclone Martin}}
-On October 27, the FMS started to monitor a weak [[tropical disturbance]] that had developed to the north of the Northern [[Cook Islands]].<ref name="97-98 ATCR"/> Over the next few days [[atmospheric convection]] surrounding the system remained disorganised, as the system moved to the southwest and was affected by strong upper-level north-easterly winds and moderate to strong [[vertical wind shear]].<ref name="1997-98 BoM"/><ref name="GP1097">{{cite web|author=Padgett, Gary |accessdate=July 23, 2013 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9710.htm |title=Monthly Global Tropical Cyclone Summary October 1997 |year=1997 |archiveurl=http://www.webcitation.org/6IKYe4gpY?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9710.htm |archivedate=July 23, 2013 |deadurl=no |df=mdy }}</ref> Late on October 30, the NPMOC designated the disturbance as Tropical Cyclone 04P, after it had developed into a tropical depression.<ref name="GP1097"/><ref>{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97103018.wrn |date=October 30, 1997 |title=Tropical Cyclone 04P Warning 1 October 30, 1997 21z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/69mzF9dtF?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97103018.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=August 9, 2012 |archivedate=August 9, 2012 |deadurl=no |df=mdy }}</ref><ref name="JTWC ATCR">{{cite report|type=1998 Annual Tropical Cyclone Report |title=Chapter 4 Summary of South Pacific and South Indian Tropical Cyclones |archivedate=July 24, 2013 |deadurl=no |author=Joint Typhoon Warning Center |publisher=United States Navy, United States Airforce |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1998atcr.pdf |year=1998 |accessdate=July 23, 2013 |pages=128 |author2=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6IL30At18?url=http%3A%2F%2Fwww.usno.navy.mil%2FNOOC%2Fnmfc-ph%2FRSS%2Fjtwc%2Fatcr%2F1998atcr.pdf |df=mdy }}</ref> During the next day the system started to show a marked improvement in organisation and began rapidly developing, before RSMC Nadi named it Martin at 1500&nbsp;UTC after it had developed into a category 1 tropical cyclone.<ref name="97-98 ATCR"/> When it was named, Martin was located about {{Convert|500|km|mi|abbr=on|disp=5}} to the west of [[Manihiki|Manihiki Atoll]] in the [[Northern Cook Islands]] and had started to re-curve and move towards the south-east during that day.<ref name="97-98 ATCR"/>{{TCWC Wellington BT}}<ref>{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110106.wrn |date=November 1, 1997 |title=Tropical Cyclone 04P (Martin) Warning 4 November 1, 1997 09z |author=Naval Pacific Meteorology and Oceanography Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXELvbeL?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97110106.wrn |accessdate=August 1, 2013 |archivedate=August 1, 2013 |deadurl=no |df=mdy }}</ref> Early on November 1, RSMC Nadi reported that the system had become a category 2 tropical cyclone on the Australian scale, before the NPMOC reported that Martin had become equivalent to a category 1 hurricane on the SSHWS.<ref name="Wellington BT"/><ref name="NPMOC Martin BT">{{cite report|type=|accessdate=July 23, 2013|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 04P (Martin) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh041998.txt|author=Naval Pacific Meteorology and Oceanography Center|author2=Joint Typhoon Warning Center}}</ref>
+On October 27, the FMS started to monitor a weak [[tropical disturbance]] that had developed to the north of the Northern [[Cook Islands]].<ref name="97-98 ATCR"/> Over the next few days [[atmospheric convection]] surrounding the system remained disorganised, as the system moved to the southwest and was affected by strong upper-level north-easterly winds and moderate to strong [[vertical wind shear]].<ref name="1997-98 BoM"/><ref name="GP1097">{{cite web|author=Padgett, Gary |accessdate=July 23, 2013 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9710.htm |title=Monthly Global Tropical Cyclone Summary October 1997 |year=1997 |archiveurl=http://www.webcitation.org/6IKYe4gpY?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9710.htm |archivedate=July 23, 2013 |deadurl=no |df=mdy }}</ref> Late on October 30, the NPMOC designated the disturbance as Tropical Cyclone 04P, after it had developed into a tropical depression.<ref name="GP1097"/><ref>{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97103018.wrn |date=October 30, 1997 |title=Tropical Cyclone 04P Warning 1 October 30, 1997 21z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/69mzF9dtF?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97103018.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=August 9, 2012 |archivedate=August 9, 2012 |deadurl=no |df=mdy }}</ref><ref name="JTWC ATCR">{{cite report|type=1998 Annual Tropical Cyclone Report |title=Chapter 4 Summary of South Pacific and South Indian Tropical Cyclones |archivedate=July 24, 2013 |deadurl=no |author=Joint Typhoon Warning Center |publisher=United States Navy, United States Airforce |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1998atcr.pdf |year=1998 |accessdate=July 23, 2013 |pages=128 |author2=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6IL30At18?url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1998atcr.pdf |df=mdy }}</ref> During the next day the system started to show a marked improvement in organisation and began rapidly developing, before RSMC Nadi named it Martin at 1500&nbsp;UTC after it had developed into a category 1 tropical cyclone.<ref name="97-98 ATCR"/> When it was named, Martin was located about {{Convert|500|km|mi|abbr=on|disp=5}} to the west of [[Manihiki|Manihiki Atoll]] in the [[Northern Cook Islands]] and had started to re-curve and move towards the south-east during that day.<ref name="97-98 ATCR"/>{{TCWC Wellington BT}}<ref>{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110106.wrn |date=November 1, 1997 |title=Tropical Cyclone 04P (Martin) Warning 4 November 1, 1997 09z |author=Naval Pacific Meteorology and Oceanography Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXELvbeL?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110106.wrn |accessdate=August 1, 2013 |archivedate=August 1, 2013 |deadurl=no |df=mdy }}</ref> Early on November 1, RSMC Nadi reported that the system had become a category 2 tropical cyclone on the Australian scale, before the NPMOC reported that Martin had become equivalent to a category 1 hurricane on the SSHWS.<ref name="Wellington BT"/><ref name="NPMOC Martin BT">{{cite report|type=|accessdate=July 23, 2013|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 04P (Martin) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh041998.txt|author=Naval Pacific Meteorology and Oceanography Center|author2=Joint Typhoon Warning Center}}</ref>
-During November 2, the system continued to intensify as it moved towards the southeast and became equivalent to a category 2 hurricane on the SSHWS, as it moved towards the [[French Polynesia]]n [[Society Islands]] of [[Motu One (Society Islands)|Bellingshausen]], [[Mopelia]] and [[Scilly]].<ref name="1997-98 BoM"/><ref name="Wellington BT"/><ref name="NPMOC Martin BT"/> During the next day, Martin passed near the Society Islands as it developed an {{convert|17|km|mi|disp=5|abbr=on}} eye, before RSMC Nadi reported at 06:00&nbsp;UTC that the system had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind speeds of 155&nbsp;km/h (100&nbsp;mph).<ref name="1997-98 BoM"/><ref name="97-98 BT"/><ref name="NPMOC AD 8">{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110306.wrn |date=November 3, 1997 |author=Naval Pacific Meteorology and Oceanography Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXElECaK?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97110306.wrn |accessdate=August 1, 2013 |archivedate=August 1, 2013 |deadurl=no |title=Tropical Cyclone 04P (Martin) Warning 8 November 3, 1997 09z |df=mdy }}</ref> The NPMOC also reported at around that time that Martin had peaked with 1-minute sustained windspeeds of 185&nbsp;km/h (115&nbsp;mph), which made it equivalent to a category 3 hurricane on the SSHWS.<ref name="NPMOC Martin BT"/><ref name="NPMOC AD 8"/> After peaking in intensity Martin started to weaken, as it interacted with a frontal system and started to accelerate towards the south-southeast.<ref name="97-98 ATCR"/><ref name="NPMOC AD 9">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110318.wrn |deadurl=no |date=November 3, 1997 |accessdate=August 1, 2013 |title=Tropical Cyclone 04P (Martin) Warning 9 November 3, 1997 21z |archiveurl=http://www.webcitation.org/6IXHmZYmM?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97110318.wrn |archivedate=August 1, 2013 |publisher=United States Navy, United States Air Force |df=mdy }}</ref> During November 4, Martin passed within {{Convert|250|km|mi|abbr=on}} of Tahiti as it became a category 2 tropical cyclone and started to transition into an extratropical cyclone.<ref name="97-98 ATCR"/><ref name="97-98 BT"/><ref name="NPMOC AD 10">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110406.wrn |date=November 4, 1997 |accessdate=August 1, 2013 |archivedate=August 1, 2013 |title=Tropical Cyclone 04P (Martin) Warning 10 November 4, 1997 03z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXHmZYmM?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97110318.wrn |df=mdy }}</ref> Later that day, the NPMOC issued their final advisory on system as it had become equivalent to a tropical depression, vertically sheared with its surface center dislocated about {{convert|110|km|mi|disp=5|abbr=on}} from its upper level center.<ref name="NPMOC Martin BT"/><ref name="NPMOC AD 11">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |title=Tropical Cyclone 04P (Martin) Warning 11 November 4, 1997 21z |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110418.wrn |date=November 4, 1997 |accessdate=August 1, 2013 |archivedate=August 1, 2013 |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXIM9W1N?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh041998.97110418.wrn |df=mdy }}</ref> During November 5, Martin weakened below tropical cyclone intensity as it moved into TCWC Wellington's area of responsibility before the system was last noted on November 8.<ref name="97-98 ATCR"/><ref name="Wellington BT"/>
+During November 2, the system continued to intensify as it moved towards the southeast and became equivalent to a category 2 hurricane on the SSHWS, as it moved towards the [[French Polynesia]]n [[Society Islands]] of [[Motu One (Society Islands)|Bellingshausen]], [[Mopelia]] and [[Scilly]].<ref name="1997-98 BoM"/><ref name="Wellington BT"/><ref name="NPMOC Martin BT"/> During the next day, Martin passed near the Society Islands as it developed an {{convert|17|km|mi|disp=5|abbr=on}} eye, before RSMC Nadi reported at 06:00&nbsp;UTC that the system had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind speeds of 155&nbsp;km/h (100&nbsp;mph).<ref name="1997-98 BoM"/><ref name="97-98 BT"/><ref name="NPMOC AD 8">{{cite report|type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110306.wrn |date=November 3, 1997 |author=Naval Pacific Meteorology and Oceanography Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXElECaK?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110306.wrn |accessdate=August 1, 2013 |archivedate=August 1, 2013 |deadurl=no |title=Tropical Cyclone 04P (Martin) Warning 8 November 3, 1997 09z |df=mdy }}</ref> The NPMOC also reported at around that time that Martin had peaked with 1-minute sustained windspeeds of 185&nbsp;km/h (115&nbsp;mph), which made it equivalent to a category 3 hurricane on the SSHWS.<ref name="NPMOC Martin BT"/><ref name="NPMOC AD 8"/> After peaking in intensity Martin started to weaken, as it interacted with a frontal system and started to accelerate towards the south-southeast.<ref name="97-98 ATCR"/><ref name="NPMOC AD 9">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110318.wrn |deadurl=no |date=November 3, 1997 |accessdate=August 1, 2013 |title=Tropical Cyclone 04P (Martin) Warning 9 November 3, 1997 21z |archiveurl=http://www.webcitation.org/6IXHmZYmM?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110318.wrn |archivedate=August 1, 2013 |publisher=United States Navy, United States Air Force |df=mdy }}</ref> During November 4, Martin passed within {{Convert|250|km|mi|abbr=on}} of Tahiti as it became a category 2 tropical cyclone and started to transition into an extratropical cyclone.<ref name="97-98 ATCR"/><ref name="97-98 BT"/><ref name="NPMOC AD 10">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110406.wrn |date=November 4, 1997 |accessdate=August 1, 2013 |archivedate=August 1, 2013 |title=Tropical Cyclone 04P (Martin) Warning 10 November 4, 1997 03z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXHmZYmM?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110318.wrn |df=mdy }}</ref> Later that day, the NPMOC issued their final advisory on system as it had become equivalent to a tropical depression, vertically sheared with its surface center dislocated about {{convert|110|km|mi|disp=5|abbr=on}} from its upper level center.<ref name="NPMOC Martin BT"/><ref name="NPMOC AD 11">{{cite report|author=Naval Pacific Meteorology and Oceanography Center |type= |title=Tropical Cyclone 04P (Martin) Warning 11 November 4, 1997 21z |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110418.wrn |date=November 4, 1997 |accessdate=August 1, 2013 |archivedate=August 1, 2013 |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6IXIM9W1N?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh041998.97110418.wrn |df=mdy }}</ref> During November 5, Martin weakened below tropical cyclone intensity as it moved into TCWC Wellington's area of responsibility before the system was last noted on November 8.<ref name="97-98 ATCR"/><ref name="Wellington BT"/>
 {{Clear}}
@@ Line 181: / Line 181: @@
 }}
-On November 15, the United States Armed Forces started to monitor a tropical disturbance, that had developed within the South Pacific Convergence Zone about 1000&nbsp;km (620&nbsp;mi) to the northeast of [[Suva|Suva, Fiji]].<ref name="05P BT">{{cite web|publisher=United States Navy, United States Air Force|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh051998.txt|title=Tropical Cyclone 05P (Nute) best track analysis|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|accessdate=May 30, 2011|year=2002}}</ref><ref name="DTDSNOV97">{{cite journal|year=1997|title=November 1997|journal=Darwin Tropical Diagnostic Statement|volume=16|issue=11|page=2|issn=1321-4233|accessdate=March 1, 2012|publisher=Australian Bureau of Meteorology|url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199711.pdf|author=Darwin Regional Specialised Meteorological Centre}}</ref> Over the next few days the system moved towards the west, before it came under the influence of the subtropical ridge of high pressure.<ref name="05P BT"/><ref name="DTDSNOV97"/> At 0000&nbsp;UTC on November 18, RSMC Nadi reported that the system had become a tropical depression, before the JTWC issued a tropical cyclone formation alert on the depression while it was located about 100&nbsp;km (60&nbsp;mi), to the southwest of the [[Solomon Island]]: [[Santa Cruz Islands|Santa Cruz]].<ref name="Nute TCR">{{cite web|title=Tropical Cyclone Nute|author=Brisbane Tropical Cyclone Warning Center|year=2010|url=http://www.bom.gov.au/cyclone/history/nute.shtml|publisher=Australian Bureau of Meteorology|accessdate=May 30, 2011}}</ref><ref name="05P AD">{{cite web|year=1997 |publisher=Australian Severe Weather |accessdate=May 30, 2011 |url=http://www.australiasevereweather.com.au/tropical_cyclones/1997_1998/warnings/tropical_cyclone_nute_jtwc_advisories.htm |author=Joint Typhoon Warning Center |title=Tropical Cyclone 05P (Nute) Advisories |archiveurl=http://www.webcitation.org/68wUvvKb2?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Ftropical_cyclones%2F1997_1998%2Fwarnings%2Ftropical_cyclone_nute_jtwc_advisories.htm |archivedate=July 6, 2012 |deadurl=no |df=mdy }}</ref> The JTWC initiated advisories on the depression at 0600&nbsp;UTC and designated it as 05P, before six hours later, RSMC Nadi named the depression Nute, as it had intensified into a category one tropical cyclone.<ref name="97-98 ATCR"/><ref name="05P AD"/> Over the next day, Nute continued to intensify and developed an eye feature before at 0600&nbsp;UTC on November 19, as the system approached 160°E, RSMC Nadi reported that Nute, had peaked as a category two tropical cyclone with 10-minute sustained wind speeds of 110&nbsp;km/h (70&nbsp;mph).<ref name="97-98 ATCR"/><ref name="Nute TCR"/> During that day RSMC Nadi reported that Nute was holding on to its peak intensity, while the JTWC reported at 1800&nbsp;UTC that Nute had reached its 1-minute peak intensity of 140&nbsp;km/h (85&nbsp;mph) as it was entering the Australian region.<ref name="GP Nov">{{cite report|title=Monthly Global Tropical Cyclone Summary November 1997 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm |accessdate=November 11, 2012 |author=Padgett, Gary |archiveurl=http://www.webcitation.org/6CQhbsBK8?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9711.htm |archivedate=November 25, 2012 |deadurl=no |df=mdy }}</ref><ref name="05P BT"/> As Nute traversed an island-free area of the western South Pacific, there were no deaths or impact reported.<ref name="Nute TCR"/>
+On November 15, the United States Armed Forces started to monitor a tropical disturbance, that had developed within the South Pacific Convergence Zone about 1000&nbsp;km (620&nbsp;mi) to the northeast of [[Suva|Suva, Fiji]].<ref name="05P BT">{{cite web|publisher=United States Navy, United States Air Force|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh051998.txt|title=Tropical Cyclone 05P (Nute) best track analysis|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|accessdate=May 30, 2011|year=2002}}</ref><ref name="DTDSNOV97">{{cite journal|year=1997|title=November 1997|journal=Darwin Tropical Diagnostic Statement|volume=16|issue=11|page=2|issn=1321-4233|accessdate=March 1, 2012|publisher=Australian Bureau of Meteorology|url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199711.pdf|author=Darwin Regional Specialised Meteorological Centre}}</ref> Over the next few days the system moved towards the west, before it came under the influence of the subtropical ridge of high pressure.<ref name="05P BT"/><ref name="DTDSNOV97"/> At 0000&nbsp;UTC on November 18, RSMC Nadi reported that the system had become a tropical depression, before the JTWC issued a tropical cyclone formation alert on the depression while it was located about 100&nbsp;km (60&nbsp;mi), to the southwest of the [[Solomon Island]]: [[Santa Cruz Islands|Santa Cruz]].<ref name="Nute TCR">{{cite web|title=Tropical Cyclone Nute|author=Brisbane Tropical Cyclone Warning Center|year=2010|url=http://www.bom.gov.au/cyclone/history/nute.shtml|publisher=Australian Bureau of Meteorology|accessdate=May 30, 2011}}</ref><ref name="05P AD">{{cite web|year=1997 |publisher=Australian Severe Weather |accessdate=May 30, 2011 |url=http://www.australiasevereweather.com.au/tropical_cyclones/1997_1998/warnings/tropical_cyclone_nute_jtwc_advisories.htm |author=Joint Typhoon Warning Center |title=Tropical Cyclone 05P (Nute) Advisories |archiveurl=http://www.webcitation.org/68wUvvKb2?url=http://www.australiasevereweather.com.au/tropical_cyclones/1997_1998/warnings/tropical_cyclone_nute_jtwc_advisories.htm |archivedate=July 6, 2012 |deadurl=no |df=mdy }}</ref> The JTWC initiated advisories on the depression at 0600&nbsp;UTC and designated it as 05P, before six hours later, RSMC Nadi named the depression Nute, as it had intensified into a category one tropical cyclone.<ref name="97-98 ATCR"/><ref name="05P AD"/> Over the next day, Nute continued to intensify and developed an eye feature before at 0600&nbsp;UTC on November 19, as the system approached 160°E, RSMC Nadi reported that Nute, had peaked as a category two tropical cyclone with 10-minute sustained wind speeds of 110&nbsp;km/h (70&nbsp;mph).<ref name="97-98 ATCR"/><ref name="Nute TCR"/> During that day RSMC Nadi reported that Nute was holding on to its peak intensity, while the JTWC reported at 1800&nbsp;UTC that Nute had reached its 1-minute peak intensity of 140&nbsp;km/h (85&nbsp;mph) as it was entering the Australian region.<ref name="GP Nov">{{cite report|title=Monthly Global Tropical Cyclone Summary November 1997 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm |accessdate=November 11, 2012 |author=Padgett, Gary |archiveurl=http://www.webcitation.org/6CQhbsBK8?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm |archivedate=November 25, 2012 |deadurl=yes |df=mdy }}</ref><ref name="05P BT"/> As Nute traversed an island-free area of the western South Pacific, there were no deaths or impact reported.<ref name="Nute TCR"/>
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@@ Line 197: / Line 197: @@
 }}
 {{main article|Cyclone Osea}}
-On November 22, RSMC Nadi started to monitor a tropical depression that had developed about {{Convert|465|km|mi|abbr=on|disp=5}} to the northeast of Manihiki Island.<ref name="GP Nov"/><ref name="JTWC Osea BT">{{cite web|accessdate=November 14, 2012|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 06P (Osea) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh061998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center}}</ref> Over the next two days, the depression gradually developed further.<ref name="GP Nov"/><ref name="NPMOC 1">{{cite web|deadurl=no |accessdate=November 25, 2012 |publisher=United States Navy, United States Air Force |title=Tropical Cyclone 06P (Osea) Warning 1 November 24, 1997 15z |author=Naval Pacific Meteorology and Oceanography Center |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112312.wrn |archiveurl=http://www.webcitation.org/6CAyDAmCR?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh061998.97112312.wrn |archivedate=November 14, 2012 |df=mdy }}</ref> At 1200&nbsp;UTC on November 23, the NPMOC reported that the depression had become equivalent to a tropical storm and assigned it the designation 06P, before 12 hours later RSMC Nadi named the system Osea as it had developed into a category 1 tropical cyclone.<ref name="97-98 ATCR"/><ref name="NPMOC 1"/> After developing into a tropical cyclone, Osea started moving towards the southeast.<ref name="GP Nov"/><ref name="NPMOC 4">{{cite web|deadurl=no |accessdate=November 25, 2012 |publisher=United States Navy, United States Air Force |title=Tropical Cyclone 06P (Osea) Warning 4 November 25, 1997 03z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112500.wrn |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6CQhKfrtM?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh061998.97112500.wrn |archivedate=November 25, 2012 |df=mdy }}</ref> During November 26, both agency's reported that the system had reached its peak intensity, with RSMC Nadi reporting 10-minute sustained windspeeds of 150&nbsp;km/h (90&nbsp;mph), while the NPMOC reported peak 1-minute sustained windspeeds of 165&nbsp;km/h (105&nbsp;mph).<ref name="Wellington BT"/><ref name="JTWC Osea BT"/> After it had peaked, Osea started to gradually weaken, before during November 27 the NPMOC issued their final warning on the system as it had become sheared.<ref name="NPMOC 8">{{cite web|accessdate=November 24, 2012 |publisher=United States Navy, United States Air Force |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112712.wrn |title=Tropical Cyclone 06P (Osea) Warning 8, November 27, 1997, 00z |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6CQChsoSF?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh061998.97112712.wrn |archivedate=November 24, 2012 |deadurl=no |df=mdy }}</ref> RSMC Nadi subsequently monitored Osea for another 24 hours before the system  degenerated into a depression during November 28.<ref name="97-98 ATCR"/><ref name="Wellington BT"/>
+On November 22, RSMC Nadi started to monitor a tropical depression that had developed about {{Convert|465|km|mi|abbr=on|disp=5}} to the northeast of Manihiki Island.<ref name="GP Nov"/><ref name="JTWC Osea BT">{{cite web|accessdate=November 14, 2012|publisher=United States Navy, United States Air Force|title=Tropical Cyclone 06P (Osea) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh061998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center}}</ref> Over the next two days, the depression gradually developed further.<ref name="GP Nov"/><ref name="NPMOC 1">{{cite web|deadurl=no |accessdate=November 25, 2012 |publisher=United States Navy, United States Air Force |title=Tropical Cyclone 06P (Osea) Warning 1 November 24, 1997 15z |author=Naval Pacific Meteorology and Oceanography Center |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112312.wrn |archiveurl=http://www.webcitation.org/6CAyDAmCR?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112312.wrn |archivedate=November 14, 2012 |df=mdy }}</ref> At 1200&nbsp;UTC on November 23, the NPMOC reported that the depression had become equivalent to a tropical storm and assigned it the designation 06P, before 12 hours later RSMC Nadi named the system Osea as it had developed into a category 1 tropical cyclone.<ref name="97-98 ATCR"/><ref name="NPMOC 1"/> After developing into a tropical cyclone, Osea started moving towards the southeast.<ref name="GP Nov"/><ref name="NPMOC 4">{{cite web|deadurl=no |accessdate=November 25, 2012 |publisher=United States Navy, United States Air Force |title=Tropical Cyclone 06P (Osea) Warning 4 November 25, 1997 03z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112500.wrn |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6CQhKfrtM?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112500.wrn |archivedate=November 25, 2012 |df=mdy }}</ref> During November 26, both agency's reported that the system had reached its peak intensity, with RSMC Nadi reporting 10-minute sustained windspeeds of 150&nbsp;km/h (90&nbsp;mph), while the NPMOC reported peak 1-minute sustained windspeeds of 165&nbsp;km/h (105&nbsp;mph).<ref name="Wellington BT"/><ref name="JTWC Osea BT"/> After it had peaked, Osea started to gradually weaken, before during November 27 the NPMOC issued their final warning on the system as it had become sheared.<ref name="NPMOC 8">{{cite web|accessdate=November 24, 2012 |publisher=United States Navy, United States Air Force |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112712.wrn |title=Tropical Cyclone 06P (Osea) Warning 8, November 27, 1997, 00z |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/6CQChsoSF?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh061998.97112712.wrn |archivedate=November 24, 2012 |deadurl=no |df=mdy }}</ref> RSMC Nadi subsequently monitored Osea for another 24 hours before the system  degenerated into a depression during November 28.<ref name="97-98 ATCR"/><ref name="Wellington BT"/>
-While it was active, Osea caused no deaths but was quite destructive to some of the northwestern Society Islands, with over 700&nbsp;homes destroyed or severely damaged on Maupiti, Bora-Bora, and [[Raiatea]].<ref name="1997-98 BoM"/> On Maupiti, an island with a population of 1,100, about 95% of the infrastructure was destroyed. The [[town hall]], two&nbsp;schools, and an airfield were destroyed.<ref name="GP">{{cite report|url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm|accessdate=November 11, 2012|author=Padgett, Gary|title=Monthly Global Tropical Cyclone Summary November 1997}}</ref> The town hall was evacuated due to the strong winds.<ref name=elninohavoc>{{cite web|title=Powerful El Nino Causing Havoc in Pacific|url=http://www.indigenousportal.com/es/Cambio-Clim%C3%A1tico/POWERFUL-EL-NINO-CAUSING-HAVOC-IN-PACIFIC.html|publisher=International Indigenous ICT Task Force|accessdate=November 25, 2012|location=Papeete, Tahiti|date=February 24, 2010}}</ref> In addition, 77&nbsp;homes on the island were destroyed.<ref name=FP1>{{cite book|title=The Ensign of the Church of Jesus Christ of Latter-Day Saints, Volume 28|year=1998|publisher=The Church}}</ref> Due to flooding, many highways were blocked.<ref name=TU>{{cite news|title=Tropical Storms|url=https://news.google.com/newspapers?id=R6U_AAAAIBAJ&sjid=YFYMAAAAIBAJ&pg=5858,295543&dq=cyclone+osea&hl=en|accessdate=November 11, 2012|newspaper=Times-Union|date=December 7, 1997}}</ref> On Bora-Bora, an island which had a population of 4,500 at the time, roughly 30% of the infrastructure was destroyed, including 309&nbsp;houses.<ref name="GP Nov"/> On the north side of Bora Bora, nearly everything was destroyed, including the village of [[Vaitape]].<ref name=ON>{{cite web|title=Powerful cyclones pound South Pacific islands|url=http://www.oceannavigator.com/January-February-2003/Powerful-cyclones-pound-South-Pacific-islands/|publisher=Oceanavaigator.com|accessdate=November 11, 2012}}</ref> In Vaitape, roads were blocked and telecommunication lines were hampered. Seven&nbsp;people on the island were injured.<ref name=sweeps>{{cite news|archivedate=November 25, 2012 |url=http://archives.pireport.org/archive/1997/november/11-26-up.html |title=Cyclone Osea sweeps through French Polynesia |date=November 26, 1997 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |author=Pacific Islands Report |accessdate=November 25, 2012 |archiveurl=http://www.webcitation.org/6CQkC7LRY?url=http%3A%2F%2Farchives.pireport.org%2Farchive%2F1997%2Fnovember%2F11%252D26%252Dup.html |deadurl=no |df=mdy }}</ref><ref>{{cite news|newspaper=[[Les Échos (Mali)|Les Échos]]|date=November 28, 1997|title=7 blesses apres le passage d'Osea|publisher=Le Monde}} (accessed via Lexis Nexis on November 25, 2012)</ref> Overall, 700&nbsp;homes were at least somewhat destroyed by Osea.<ref name="PacificIslanders1997">{{cite news|title=Pacific Islanders confident of surviving Cyclone Pam|newspaper=Agence France Presse|date=December 8, 1997}}</ref> Throughout French Polynesia, [[banana tree]]s were knocked down due to the strong winds.<ref name=drylanhorticulture>{{cite web|title=Dryland Horticulture in Maupiti: An Ethnoarchaeological Study|url=http://scholarspace.manoa.hawaii.edu/bitstream/handle/10125/17175/AP-v41n2-269-283.pdf?sequence=1|publisher=University of Hawai'i Press|accessdate=November 25, 2012|author=Cauchois, Mickaelle-Hinanui|author2=Service du Patrimoine, Ministere de la Culture|page=277|year=2002}}</ref>
+While it was active, Osea caused no deaths but was quite destructive to some of the northwestern Society Islands, with over 700&nbsp;homes destroyed or severely damaged on Maupiti, Bora-Bora, and [[Raiatea]].<ref name="1997-98 BoM"/> On Maupiti, an island with a population of 1,100, about 95% of the infrastructure was destroyed. The [[town hall]], two&nbsp;schools, and an airfield were destroyed.<ref name="GP">{{cite report|url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm |accessdate=November 11, 2012 |author=Padgett, Gary |title=Monthly Global Tropical Cyclone Summary November 1997 |deadurl=yes |archiveurl=http://www.webcitation.org/6CQhbsBK8?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9711.htm |archivedate=November 25, 2012 |df= }}</ref> The town hall was evacuated due to the strong winds.<ref name=elninohavoc>{{cite web|title=Powerful El Nino Causing Havoc in Pacific|url=http://www.indigenousportal.com/es/Cambio-Clim%C3%A1tico/POWERFUL-EL-NINO-CAUSING-HAVOC-IN-PACIFIC.html|publisher=International Indigenous ICT Task Force|accessdate=November 25, 2012|location=Papeete, Tahiti|date=February 24, 2010}}</ref> In addition, 77&nbsp;homes on the island were destroyed.<ref name=FP1>{{cite book|title=The Ensign of the Church of Jesus Christ of Latter-Day Saints, Volume 28|year=1998|publisher=The Church}}</ref> Due to flooding, many highways were blocked.<ref name=TU>{{cite news|title=Tropical Storms|url=https://news.google.com/newspapers?id=R6U_AAAAIBAJ&sjid=YFYMAAAAIBAJ&pg=5858,295543&dq=cyclone+osea&hl=en|accessdate=November 11, 2012|newspaper=Times-Union|date=December 7, 1997}}</ref> On Bora-Bora, an island which had a population of 4,500 at the time, roughly 30% of the infrastructure was destroyed, including 309&nbsp;houses.<ref name="GP Nov"/> On the north side of Bora Bora, nearly everything was destroyed, including the village of [[Vaitape]].<ref name=ON>{{cite web|title=Powerful cyclones pound South Pacific islands|url=http://www.oceannavigator.com/January-February-2003/Powerful-cyclones-pound-South-Pacific-islands/|publisher=Oceanavaigator.com|accessdate=November 11, 2012}}</ref> In Vaitape, roads were blocked and telecommunication lines were hampered. Seven&nbsp;people on the island were injured.<ref name=sweeps>{{cite news|archivedate=November 25, 2012 |url=http://archives.pireport.org/archive/1997/november/11-26-up.html |title=Cyclone Osea sweeps through French Polynesia |date=November 26, 1997 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |author=Pacific Islands Report |accessdate=November 25, 2012 |archiveurl=http://www.webcitation.org/6CQkC7LRY?url=http://archives.pireport.org/archive/1997/november/11-26-up.html |deadurl=no |df=mdy }}</ref><ref>{{cite news|newspaper=[[Les Échos (Mali)|Les Échos]]|date=November 28, 1997|title=7 blesses apres le passage d'Osea|publisher=Le Monde}} (accessed via Lexis Nexis on November 25, 2012)</ref> Overall, 700&nbsp;homes were at least somewhat destroyed by Osea.<ref name="PacificIslanders1997">{{cite news|title=Pacific Islanders confident of surviving Cyclone Pam|newspaper=Agence France Presse|date=December 8, 1997}}</ref> Throughout French Polynesia, [[banana tree]]s were knocked down due to the strong winds.<ref name=drylanhorticulture>{{cite web|title=Dryland Horticulture in Maupiti: An Ethnoarchaeological Study|url=http://scholarspace.manoa.hawaii.edu/bitstream/handle/10125/17175/AP-v41n2-269-283.pdf?sequence=1|publisher=University of Hawai'i Press|accessdate=November 25, 2012|author=Cauchois, Mickaelle-Hinanui|author2=Service du Patrimoine, Ministere de la Culture|page=277|year=2002}}</ref>
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-At the end of November, an equatorial [[westerly wind burst]], occurred about {{convert|2000|km|mi|disp=5|abbr=on}} to the south-west of [[Hawaii]]. This wind burst led to the development of two [[tropical cyclones]], to the east of the [[International Dateline]] on either side of the [[equator]].<ref name="1997-98 BoM"/> During December 5, both RSMC Nadi and the NPMOC started to monitor the system as a tropical depression, while it was located between the [[Samoan Islands|Samoa]]n and [[Cook Islands|Northern Cook]] Islands.<ref name="1997-98 BoM"/><ref name="Dec 97"/><ref>{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 23, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120518.wrn |title=Tropical Cyclone 07P Warning 1 December 6, 1997 21z |archiveurl=http://www.webcitation.org/6Nad0UhJp?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh071998.97120518.wrn |accessdate=February 23, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> During that day the system slowly developed and organized further and moved south-eastwards, before early on December 6, RSMC Nadi reported that the system had developed into a category 1 tropical cyclone and named it Pam.<ref name="97-98 ATCR"/><ref name="Dec 97">{{cite web|title=Monthly Global Tropical Cyclone Summary December 1997 |author=Padgett, Gary |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9712.htm |accessdate=February 22, 2014 |archiveurl=http://www.webcitation.org/6NaNk7nox?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9712.htm |archivedate=February 22, 2014 |deadurl=no |df=mdy }}</ref> After it was named the system continued to slowly drift towards the south-southeast, before it started to move quicker later that day as it passed near the [[Cook Islands|Cook Island]] of [[Suwarrow]].<ref name="Dec 97"/> As the system passed near Suwarrow, the NPMOC reported that Pam had reached its peak intensity with 1-minute sustained wind speeds of 120&nbsp;km/h (75&nbsp;mph), which made it equivalent to a category 1 hurricane on the SSHWS.<ref name="07P BT">{{cite web|accessdate=February 23, 2014|publisher=United States Navy, United States Air Force|author=Joint Typhoon Warning Center|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh071998.txt|title=Tropical Cyclone 07P (Pam) best track analysis}}</ref>
+At the end of November, an equatorial [[westerly wind burst]], occurred about {{convert|2000|km|mi|disp=5|abbr=on}} to the south-west of [[Hawaii]]. This wind burst led to the development of two [[tropical cyclones]], to the east of the [[International Dateline]] on either side of the [[equator]].<ref name="1997-98 BoM"/> During December 5, both RSMC Nadi and the NPMOC started to monitor the system as a tropical depression, while it was located between the [[Samoan Islands|Samoa]]n and [[Cook Islands|Northern Cook]] Islands.<ref name="1997-98 BoM"/><ref name="Dec 97"/><ref>{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 23, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120518.wrn |title=Tropical Cyclone 07P Warning 1 December 6, 1997 21z |archiveurl=http://www.webcitation.org/6Nad0UhJp?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120518.wrn |accessdate=February 23, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> During that day the system slowly developed and organized further and moved south-eastwards, before early on December 6, RSMC Nadi reported that the system had developed into a category 1 tropical cyclone and named it Pam.<ref name="97-98 ATCR"/><ref name="Dec 97">{{cite web|title=Monthly Global Tropical Cyclone Summary December 1997 |author=Padgett, Gary |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9712.htm |accessdate=February 22, 2014 |archiveurl=http://www.webcitation.org/6NaNk7nox?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9712.htm |archivedate=February 22, 2014 |deadurl=no |df=mdy }}</ref> After it was named the system continued to slowly drift towards the south-southeast, before it started to move quicker later that day as it passed near the [[Cook Islands|Cook Island]] of [[Suwarrow]].<ref name="Dec 97"/> As the system passed near Suwarrow, the NPMOC reported that Pam had reached its peak intensity with 1-minute sustained wind speeds of 120&nbsp;km/h (75&nbsp;mph), which made it equivalent to a category 1 hurricane on the SSHWS.<ref name="07P BT">{{cite web|accessdate=February 23, 2014|publisher=United States Navy, United States Air Force|author=Joint Typhoon Warning Center|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh071998.txt|title=Tropical Cyclone 07P (Pam) best track analysis}}</ref>
-Over the next couple of days the system moved southwards before RSMC Nadi reported during December 8, that Pam had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind-speeds of {{convert|120|km/h|mph|disp=5|abbr=on}}.<ref name="Dec 97"/><ref name="Dec tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks December 1997 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9712.htm |archiveurl=http://www.webcitation.org/6NbRq2wow?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Ftrak9712.htm |author=Padgett, Gary |archivedate=February 23, 2014 |deadurl=no |df=mdy }}</ref> However, during the systems post analysis, RSMC Nadi reduced these winds slightly to {{convert|110|km/h|mph|disp=5|abbr=on}} which made Pam a category 2 tropical cyclone, rather than a category 3 severe tropical cyclone on the Australian scale.<ref name="Wellington BT"/><ref name="Dec tracks"/> During December 8, the system passed about {{convert|140|km|mi|disp=5|abbr=on}} to the east of Palmerston Island, before it passed about {{convert|75|km|mi|disp=5|abbr=on}} to the southwest of Rarotonga early the next day.<ref name="Dec 97"/> During December 9, Pam started to rapidly weaken as it transitioned into an extra-tropical cyclone, while RSMC Nadi reported during the next day that the system had degenerated into depression.<ref name="Dec 97"/><ref>{{cite web|publisher=United States Navy, United States Air Force |author=Joint Typhoon Warning Center |archivedate=February 23, 2014 |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120918.wrn |title=Tropical Cyclone 07P (Pam) Warning 9 December 9, 1997 21z |archiveurl=http://www.webcitation.org/6NbT9e0z1?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh071998.97120918.wrn |accessdate=February 23, 2014 |df=mdy }}</ref> Over the next few days the system continued to move southeastwards, before it was last noted during December 14, while located to the west of Chile.<ref name="Wellington BT"/>
+Over the next couple of days the system moved southwards before RSMC Nadi reported during December 8, that Pam had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind-speeds of {{convert|120|km/h|mph|disp=5|abbr=on}}.<ref name="Dec 97"/><ref name="Dec tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks December 1997 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9712.htm |archiveurl=http://www.webcitation.org/6NbRq2wow?url=http://www.australiasevereweather.com.au/cyclones/1998/trak9712.htm |author=Padgett, Gary |archivedate=February 23, 2014 |deadurl=no |df=mdy }}</ref> However, during the systems post analysis, RSMC Nadi reduced these winds slightly to {{convert|110|km/h|mph|disp=5|abbr=on}} which made Pam a category 2 tropical cyclone, rather than a category 3 severe tropical cyclone on the Australian scale.<ref name="Wellington BT"/><ref name="Dec tracks"/> During December 8, the system passed about {{convert|140|km|mi|disp=5|abbr=on}} to the east of Palmerston Island, before it passed about {{convert|75|km|mi|disp=5|abbr=on}} to the southwest of Rarotonga early the next day.<ref name="Dec 97"/> During December 9, Pam started to rapidly weaken as it transitioned into an extra-tropical cyclone, while RSMC Nadi reported during the next day that the system had degenerated into depression.<ref name="Dec 97"/><ref>{{cite web|publisher=United States Navy, United States Air Force |author=Joint Typhoon Warning Center |archivedate=February 23, 2014 |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120918.wrn |title=Tropical Cyclone 07P (Pam) Warning 9 December 9, 1997 21z |archiveurl=http://www.webcitation.org/6NbT9e0z1?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh071998.97120918.wrn |accessdate=February 23, 2014 |df=mdy }}</ref> Over the next few days the system continued to move southeastwards, before it was last noted during December 14, while located to the west of Chile.<ref name="Wellington BT"/>
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 {{Main article|Cyclone Susan}}
-On December 20, RSMC Nadi started to monitor a weak [[tropical disturbance]], that was located about to the north of Tuvalu.<ref name="Jan 98">{{cite report|author=Padgett, Gary|url=http://australiasevereweather.com/cyclones/1998/summ9801.htm|title=Monthly Global Tropical Cyclone Summary January 1998|accessdate=January 21, 2015|type=}}</ref><ref name="11P BT">{{cite web|publisher=United States Navy, United States Air Force |author2=Naval Pacific Meteorology and Oceanography Center |author1=Joint Typhoon Warning Center |archivedate=January 1, 2012 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh111998.txt |archiveurl=http://www.webcitation.org/64NPmi6lo?url=http%3A%2F%2Fwww.usno.navy.mil%2FNOOC%2Fnmfc-ph%2FRSS%2Fjtwc%2Fbest_tracks%2F1998%2F1998s-bsh%2Fbsh111998.txt |deadurl=no |accessdate=February 28, 2014 |title=Tropical Cyclone 11P (Susan) best track analysis |df=mdy }}</ref> Over the next two weeks the system gradually moved towards the west-southwest, without developing into a tropical cyclone.<ref name="Jan 98"/> During January 3, the JTWC initiated warnings on the system and designated it as Tropical Cyclone 11P.<ref>{{cite web|date=January 3, 1998 |title=Tropical Cyclone 11P (Susan) Warning 1 January 3, 1998 0000z |publisher=United States Navy, United States Air Force |accessdate=July 18, 2011 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010300.wrn |archiveurl=http://www.webcitation.org/64NNbjvQS?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh111998.98010300.wrn |archivedate=January 1, 2012 |deadurl=no |author=Joint Typhoon Warning Center |df=mdy }}</ref> Later that day RSMC Nadi named the system Susan as the system had become a category 1 tropical cyclone, while it was located near the Fiji dependency of [[Rotuma]].<ref name="Susan Prem report">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |title=Preliminary Report on Tropical Cyclone Susan&nbsp;— January 3 - 9, 1998 |publisher=Fiji Meteorological Service |date=January 20, 1998 |accessdate=December 14, 2013 |url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_TC_1998_Preliminary_report.pdf |archiveurl=http://www.webcitation.org/6LryJ3hi2?url=http%3A%2F%2Fwww.pacificdisaster.net%2Fpdnadmin%2Fdata%2Foriginal%2FCRP_TC_1998_Preliminary_report.pdf |archivedate=December 14, 2013 |deadurl=no |df=mdy }}</ref> During that day the system continued to rapidly develop with RSMC Nadi reporting early on January 4, that Susan had become a category 3 severe tropical cyclone, with 10-minute sustained windspeeds of 120&nbsp;km/h (75&nbsp;mph).<ref name="97-98 BT"/> Later that day the JTWC reported that Susan had become equivalent to a category 1 hurricane on the [[Saffir-Simpson Hurricane Scale]], as atmospheric convection surrounding the system organized further and developed an eye feature.<ref name="11P BT"/><ref>{{cite web|title=Tropical Cyclone 11P (Susan) Warning 4, January 4, 1998 1200z|accessdate=July 18, 2011|date=January 4, 1998|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010412.wrn|author=Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force}}</ref>
+On December 20, RSMC Nadi started to monitor a weak [[tropical disturbance]], that was located about to the north of Tuvalu.<ref name="Jan 98">{{cite report|author=Padgett, Gary|url=http://australiasevereweather.com/cyclones/1998/summ9801.htm|title=Monthly Global Tropical Cyclone Summary January 1998|accessdate=January 21, 2015|type=}}</ref><ref name="11P BT">{{cite web|publisher=United States Navy, United States Air Force |author2=Naval Pacific Meteorology and Oceanography Center |author1=Joint Typhoon Warning Center |archivedate=January 1, 2012 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh111998.txt |archiveurl=http://www.webcitation.org/64NPmi6lo?url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh111998.txt |deadurl=no |accessdate=February 28, 2014 |title=Tropical Cyclone 11P (Susan) best track analysis |df=mdy }}</ref> Over the next two weeks the system gradually moved towards the west-southwest, without developing into a tropical cyclone.<ref name="Jan 98"/> During January 3, the JTWC initiated warnings on the system and designated it as Tropical Cyclone 11P.<ref>{{cite web|date=January 3, 1998 |title=Tropical Cyclone 11P (Susan) Warning 1 January 3, 1998 0000z |publisher=United States Navy, United States Air Force |accessdate=July 18, 2011 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010300.wrn |archiveurl=http://www.webcitation.org/64NNbjvQS?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010300.wrn |archivedate=January 1, 2012 |deadurl=no |author=Joint Typhoon Warning Center |df=mdy }}</ref> Later that day RSMC Nadi named the system Susan as the system had become a category 1 tropical cyclone, while it was located near the Fiji dependency of [[Rotuma]].<ref name="Susan Prem report">{{cite report|author=RSMC Nadi&nbsp;— Tropical Cyclone Centre |title=Preliminary Report on Tropical Cyclone Susan&nbsp;— January 3 - 9, 1998 |publisher=Fiji Meteorological Service |date=January 20, 1998 |accessdate=December 14, 2013 |url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_TC_1998_Preliminary_report.pdf |archiveurl=http://www.webcitation.org/6LryJ3hi2?url=http://www.pacificdisaster.net/pdnadmin/data/original/CRP_TC_1998_Preliminary_report.pdf |archivedate=December 14, 2013 |deadurl=yes |df=mdy }}</ref> During that day the system continued to rapidly develop with RSMC Nadi reporting early on January 4, that Susan had become a category 3 severe tropical cyclone, with 10-minute sustained windspeeds of 120&nbsp;km/h (75&nbsp;mph).<ref name="97-98 BT"/> Later that day the JTWC reported that Susan had become equivalent to a category 1 hurricane on the [[Saffir-Simpson Hurricane Scale]], as atmospheric convection surrounding the system organized further and developed an eye feature.<ref name="11P BT"/><ref>{{cite web|title=Tropical Cyclone 11P (Susan) Warning 4, January 4, 1998 1200z|accessdate=July 18, 2011|date=January 4, 1998|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010412.wrn|author=Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force}}</ref>
-Susan subsequently moved towards the southwest as the subtropical ridge of high pressure weakened.<ref name="DTDSJAN98">{{cite journal|year=1998|title=January 1998|journal=Darwin Tropical Diagnostic Statement|publisher=Bureau of Meteorology|location=Australian|volume=17|issue=1|author=Darwin Regional Specialised Meteorological Centre|pages=2–3|issn=1321-4233|url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199801.pdf|accessdate=January 11, 2012}}</ref> Early on January 5, RSMC Nadi reported that Susan had peaked as a category 5 severe tropical cyclone with 10-minute sustained wind speeds of 140&nbsp;mph (220&nbsp;km/h),  while the JTWC reported that Susan had peaked with 1-minute wind speeds of 260&nbsp;km/h (160&nbsp;mph) equivalent to a low-end category five hurricane on the SSHS.<ref name="97-98 BT"/><ref name="11P BT"/><ref name="DTDSJAN98"/> As the system reached its peak intensity, Susan was moving towards the southwest and as a result, it "posed a severe threat to Vanuatu," however during that afternoon, Susan recurved towards the southeast "just in time to spare Vanuatu, a direct hit.”<ref name="97-98 ATCR"/> After turning away from Vanuatu, Susan accelerated towards the southeast while remaining near or at its peak intensities, before starting to weaken significantly during January 7.<ref name="97-98 BT"/> RSMC Nadi then reported early the next day, that Susan had weakened into a category 4 severe tropical cyclone while it was located about {{Convert|435|km|disp=5|abbr=on}}, to the southeast of Nadi, Fiji, which was close enough for the system to produce gale force winds in several southern and western [[Fiji|Fijian Islands]].<ref name="1997-98 BoM"/><ref name="97-98 BT"/> Later that day, Susan started to interact with [[Cyclone Ron|Ron]] before by 0000&nbsp;UTC on January 9, Susan had completely absorbed Ron.<ref name="97-98 ATCR"/> The final advisories on the combined system, were then released later that day as the system lost its tropical characteristics and started to undergo an extratropical transition.<ref name="97-98 ATCR"/><ref>{{cite web|title=Tropical Cyclone 11P (Susan) Warning 13 January 9, 1998 0300z |date=January 9, 1998 |archivedate=January 6, 2012 |deadurl=no |accessdate=July 18, 2011 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010906.wrn |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/64TjgNn1W?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh111998.98010906.wrn |author=Naval Pacific Meteorological and Oceanographic Center |df=mdy }}</ref> The remnants of the combined systems were then monitored for another day until they were last noted at 1200&nbsp;UTC on January 10, bringing an unseasonable cold snap to New Zealand.<ref name="Wellington BT"/><ref>{{cite news|date=January 10, 1998|title=Blame Cyclone Susan for cold snap|work=The Southland Times|publisher=The Southland Times Co. Ltd.|page=1|location=New Zealand}}</ref>
+Susan subsequently moved towards the southwest as the subtropical ridge of high pressure weakened.<ref name="DTDSJAN98">{{cite journal|year=1998 |title=January 1998 |journal=Darwin Tropical Diagnostic Statement |publisher=Bureau of Meteorology |location=Australian |volume=17 |issue=1 |author=Darwin Regional Specialised Meteorological Centre |pages=2–3 |issn=1321-4233 |url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199801.pdf |accessdate=January 11, 2012 |deadurl=yes |archiveurl=http://www.webcitation.org/6dEhky6Rl?url=http://www.bom.gov.au/climate/ntregion/statements/tropical/dtds-199801.pdf |archivedate=November 22, 2015 |df= }}</ref> Early on January 5, RSMC Nadi reported that Susan had peaked as a category 5 severe tropical cyclone with 10-minute sustained wind speeds of 140&nbsp;mph (220&nbsp;km/h),  while the JTWC reported that Susan had peaked with 1-minute wind speeds of 260&nbsp;km/h (160&nbsp;mph) equivalent to a low-end category five hurricane on the SSHS.<ref name="97-98 BT"/><ref name="11P BT"/><ref name="DTDSJAN98"/> As the system reached its peak intensity, Susan was moving towards the southwest and as a result, it "posed a severe threat to Vanuatu," however during that afternoon, Susan recurved towards the southeast "just in time to spare Vanuatu, a direct hit.”<ref name="97-98 ATCR"/> After turning away from Vanuatu, Susan accelerated towards the southeast while remaining near or at its peak intensities, before starting to weaken significantly during January 7.<ref name="97-98 BT"/> RSMC Nadi then reported early the next day, that Susan had weakened into a category 4 severe tropical cyclone while it was located about {{Convert|435|km|disp=5|abbr=on}}, to the southeast of Nadi, Fiji, which was close enough for the system to produce gale force winds in several southern and western [[Fiji|Fijian Islands]].<ref name="1997-98 BoM"/><ref name="97-98 BT"/> Later that day, Susan started to interact with [[Cyclone Ron|Ron]] before by 0000&nbsp;UTC on January 9, Susan had completely absorbed Ron.<ref name="97-98 ATCR"/> The final advisories on the combined system, were then released later that day as the system lost its tropical characteristics and started to undergo an extratropical transition.<ref name="97-98 ATCR"/><ref>{{cite web|title=Tropical Cyclone 11P (Susan) Warning 13 January 9, 1998 0300z |date=January 9, 1998 |archivedate=January 6, 2012 |deadurl=no |accessdate=July 18, 2011 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010906.wrn |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/64TjgNn1W?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh111998.98010906.wrn |author=Naval Pacific Meteorological and Oceanographic Center |df=mdy }}</ref> The remnants of the combined systems were then monitored for another day until they were last noted at 1200&nbsp;UTC on January 10, bringing an unseasonable cold snap to New Zealand.<ref name="Wellington BT"/><ref>{{cite news|date=January 10, 1998|title=Blame Cyclone Susan for cold snap|work=The Southland Times|publisher=The Southland Times Co. Ltd.|page=1|location=New Zealand}}</ref>
 Total damage from Susan was minor.<ref name="Jan 98"/> High seas in accordance with Susan inundated the village of Talaulia on Kadavu, Fiji. There was also some destroyed waterfront buildings, roads, jetties and bridges on Kadavu. In Beqa Island, only high seas and swells were experienced. In the town of Lautoka, on Viti Levu, roofs were blown off shops. This damage was possibly caused by a tornado that formed from one of the outer rain bands. One death was reported in accordance with Susan. This death was on Ambrym Island in [[Vanuatu]], where a woman was killed by a falling coconut palm tree.<ref name="Jan 98"/>
@@ Line 291: / Line 291: @@
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-On January 25, both RSMC Nadi and the NPMOC reported that Tropical Depression 16P, had developed about 360&nbsp;km (225&nbsp;mi) to the northwest of [[Apia, Samoa]].<ref name="97-98 ATCR"/><ref name="97-98 BT"/><ref name="JTWC ATCR"/> During that day, as the depression moved towards the southeast it gradually intensified further before at 2100&nbsp;UTC, RSMC Nadi reported that the depression had intensified into a category one tropical cyclone, and named it as Tui, while it was located about 80&nbsp;km (50&nbsp;mi) to the northwest of Apia.<ref name="97-98 ATCR"/> After it was named, Tui passed over the Samoan Islands of [[Upolu]] and [[Savai'i]], before at 0600&nbsp;UTC, both RSMC Nadi and the NPMOC reported that Tui had peaked with 10 and 1 minute sustained windspeeds of 75&nbsp;km/h (45&nbsp;mph).<ref name="97-98 BT"/><ref name="16P BT">{{cite web|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh161998.txt|title=Tropical Cyclone 16P best track analysis|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|date=December 17, 2002|publisher=United States Navy, United States Air Force|accessdate=June 2, 2011}}</ref> After it had crossed Samoa, the system remained near stationary, just to the south of Samoa, before early on January 27 both the NPMOC and RSMC Nadi, reported that Tui had weakened into a depression and issued their final advisories.<ref name="97-98 ATCR"/><ref name="Jan 98"/><ref name="16P BT"/> After Tui was downgraded to a depression, a weak circulation remained in the vicinity of the Samoan islands for several days, before it possibly redeveloped into [[#Tropical Cyclone Wes|Tropical Cyclone Wes]].<ref name="1997-98 BoM"/><ref name="97-98 ATCR"/> Ahead of Tui affecting the Samoan islands, [[Polynesian Airlines]] and [[Samoa Air]] cancelled all of their flights to the islands.<ref>{{cite news|title=Cyclone Tui heading toward Samoa|date=January 25, 1998|work=Agence France Presse}}</ref> Large crop losses and some infrastructure damage were reported in American Samoa and Western Samoa after gale force wind gusts, heavy rain and rough seas brought down power lines, trees and other debris.<ref>{{cite news|archivedate=July 26, 2011 |url=http://archives.pireport.org/archive/1998/january/01-27-08.html |title=Samoans examining damage from Cyclone Tui |date=January 27, 1998 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |author=Pacific Islands Report |accessdate=July 26, 2011 |archiveurl=http://www.webcitation.org/60SGDjQca?url=http%3A%2F%2Farchives.pireport.org%2Farchive%2F1998%2Fjanuary%2F01%252D27%252D08.html |deadurl=no |df=mdy }}</ref><ref>{{cite journal|title=January 1998 |journal=Storm Data |volume=39 |issue=1 |url=http://www1.ncdc.noaa.gov/pub/orders/IPS-5F25D463-EDE9-47CB-84B8-E4DF5CD4098B.pdf |accessdate=August 9, 2012 |author=National Climatic Data Center |editor1=Del Greco, Stephen |editor2=Hinson, Stuart |page=15 |publisher=National Environmental Satellite Data, And Information Service, National Oceanic And Atmospheric Administration |archiveurl=http://www.webcitation.org/69mLS9ooz?url=http%3A%2F%2Fwww1.ncdc.noaa.gov%2Fpub%2Forders%2FIPS-5F25D463-EDE9-47CB-84B8-E4DF5CD4098B.pdf |archivedate=August 9, 2012 |deadurl=no |df=mdy }}</ref> On the Western Samoan island of Savai'i, a young boy was killed when he stepped into an electrified puddle of water.<ref name="97-98 ATCR"/>
+On January 25, both RSMC Nadi and the NPMOC reported that Tropical Depression 16P, had developed about 360&nbsp;km (225&nbsp;mi) to the northwest of [[Apia, Samoa]].<ref name="97-98 ATCR"/><ref name="97-98 BT"/><ref name="JTWC ATCR"/> During that day, as the depression moved towards the southeast it gradually intensified further before at 2100&nbsp;UTC, RSMC Nadi reported that the depression had intensified into a category one tropical cyclone, and named it as Tui, while it was located about 80&nbsp;km (50&nbsp;mi) to the northwest of Apia.<ref name="97-98 ATCR"/> After it was named, Tui passed over the Samoan Islands of [[Upolu]] and [[Savai'i]], before at 0600&nbsp;UTC, both RSMC Nadi and the NPMOC reported that Tui had peaked with 10 and 1 minute sustained windspeeds of 75&nbsp;km/h (45&nbsp;mph).<ref name="97-98 BT"/><ref name="16P BT">{{cite web|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh161998.txt|title=Tropical Cyclone 16P best track analysis|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|date=December 17, 2002|publisher=United States Navy, United States Air Force|accessdate=June 2, 2011}}</ref> After it had crossed Samoa, the system remained near stationary, just to the south of Samoa, before early on January 27 both the NPMOC and RSMC Nadi, reported that Tui had weakened into a depression and issued their final advisories.<ref name="97-98 ATCR"/><ref name="Jan 98"/><ref name="16P BT"/> After Tui was downgraded to a depression, a weak circulation remained in the vicinity of the Samoan islands for several days, before it possibly redeveloped into [[#Tropical Cyclone Wes|Tropical Cyclone Wes]].<ref name="1997-98 BoM"/><ref name="97-98 ATCR"/> Ahead of Tui affecting the Samoan islands, [[Polynesian Airlines]] and [[Samoa Air]] cancelled all of their flights to the islands.<ref>{{cite news|title=Cyclone Tui heading toward Samoa|date=January 25, 1998|work=Agence France Presse}}</ref> Large crop losses and some infrastructure damage were reported in American Samoa and Western Samoa after gale force wind gusts, heavy rain and rough seas brought down power lines, trees and other debris.<ref>{{cite news|archivedate=July 26, 2011 |url=http://archives.pireport.org/archive/1998/january/01-27-08.html |title=Samoans examining damage from Cyclone Tui |date=January 27, 1998 |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |author=Pacific Islands Report |accessdate=July 26, 2011 |archiveurl=http://www.webcitation.org/60SGDjQca?url=http://archives.pireport.org/archive/1998/january/01-27-08.html |deadurl=no |df=mdy }}</ref><ref>{{cite journal|title=January 1998 |journal=Storm Data |volume=39 |issue=1 |url=http://www1.ncdc.noaa.gov/pub/orders/IPS-5F25D463-EDE9-47CB-84B8-E4DF5CD4098B.pdf |accessdate=August 9, 2012 |author=National Climatic Data Center |editor1=Del Greco, Stephen |editor2=Hinson, Stuart |page=15 |publisher=National Environmental Satellite Data, And Information Service, National Oceanic And Atmospheric Administration |archiveurl=http://www.webcitation.org/69mLS9ooz?url=http://www1.ncdc.noaa.gov/pub/orders/IPS-5F25D463-EDE9-47CB-84B8-E4DF5CD4098B.pdf |archivedate=August 9, 2012 |deadurl=no |df=mdy }}</ref> On the Western Samoan island of Savai'i, a young boy was killed when he stepped into an electrified puddle of water.<ref name="97-98 ATCR"/>
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-Just after Tropical Cyclone Tui had weakened into a depression near the Samoan Islands, a new tropical depression developed to the northeast of [[Tahiti]] in French Polynesia during January 29.<ref name="1997-98 BoM"/> Over the next day the system subsequently moved south-eastwards and gradually developed further, before it was declared to be a Category 1 tropical cyclone and named Ursula by the FMS.<ref name="Jan 98"/> Ursula subsequently gradually intensified and accelerated towards the south-east, as it got caught up in a westerly flow and passed through the [[Tuamotu archipelago]].<ref name="97-98 BT"/> During February 1, the system peaked as a Category 2 tropical cyclone with 10-minute wind speeds of 110&nbsp;km/h (65&nbsp;mph), before the NPMOC initiated advisories and designated Ursula as Tropical Cyclone 17P with peak 1-minute wind speeds of 120&nbsp;km/h (75&nbsp;mph).<ref name="97-98 BT"/><ref name="Jan 98"/><ref name="17P">{{cite web|title=Tropical Cyclone 17P best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh171998.txt|date=December 17, 2002|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force|accessdate=June 5, 2011}}</ref> Over the next day the system transitioned into an extratropical cyclone, before the remnants were last noted on February 5, while they were located around {{convert|4350|km|mi|disp=5|abbr=on}} to the southwest of [[Lima, Peru]].<ref name="1997-98 BoM"/><ref name="Wellington BT"/> In association with Tropical Cyclone Veli, Ursula brought significant waves which caused minor damages to three Tuamotuan islands of Mataiva, Rangiroa, Makatea.<ref name="GP March 1998">{{cite web|year=1998 |deadurl=no |title=Monthly Global Tropical Cyclone Summary March 1998 |author=Padgett, Gary |archivedate=November 28, 2015 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9803.htm |accessdate=November 28, 2015 |archiveurl=http://www.webcitation.org/6dO1Bb7dY?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9803.htm |website=Australian Severe Weather |df=mdy }}</ref> Mataiva was the worst hit island with 39 homes damaged, while roads and bridges were washed away.<ref name="GP March 1998"/> On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted, after coral and sand washed up onshore.<ref name="GP March 1998"/>
+Just after Tropical Cyclone Tui had weakened into a depression near the Samoan Islands, a new tropical depression developed to the northeast of [[Tahiti]] in French Polynesia during January 29.<ref name="1997-98 BoM"/> Over the next day the system subsequently moved south-eastwards and gradually developed further, before it was declared to be a Category 1 tropical cyclone and named Ursula by the FMS.<ref name="Jan 98"/> Ursula subsequently gradually intensified and accelerated towards the south-east, as it got caught up in a westerly flow and passed through the [[Tuamotu archipelago]].<ref name="97-98 BT"/> During February 1, the system peaked as a Category 2 tropical cyclone with 10-minute wind speeds of 110&nbsp;km/h (65&nbsp;mph), before the NPMOC initiated advisories and designated Ursula as Tropical Cyclone 17P with peak 1-minute wind speeds of 120&nbsp;km/h (75&nbsp;mph).<ref name="97-98 BT"/><ref name="Jan 98"/><ref name="17P">{{cite web|title=Tropical Cyclone 17P best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh171998.txt|date=December 17, 2002|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force|accessdate=June 5, 2011}}</ref> Over the next day the system transitioned into an extratropical cyclone, before the remnants were last noted on February 5, while they were located around {{convert|4350|km|mi|disp=5|abbr=on}} to the southwest of [[Lima, Peru]].<ref name="1997-98 BoM"/><ref name="Wellington BT"/> In association with Tropical Cyclone Veli, Ursula brought significant waves which caused minor damages to three Tuamotuan islands of Mataiva, Rangiroa, Makatea.<ref name="GP March 1998">{{cite web|year=1998 |deadurl=no |title=Monthly Global Tropical Cyclone Summary March 1998 |author=Padgett, Gary |archivedate=November 28, 2015 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9803.htm |accessdate=November 28, 2015 |archiveurl=http://www.webcitation.org/6dO1Bb7dY?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9803.htm |website=Australian Severe Weather |df=mdy }}</ref> Mataiva was the worst hit island with 39 homes damaged, while roads and bridges were washed away.<ref name="GP March 1998"/> On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted, after coral and sand washed up onshore.<ref name="GP March 1998"/>
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@@ Line 323: / Line 323: @@
 }}
-During January 30, a tropical depression developed about {{convert|650|km|mi|disp=5|abbr=on}} to the northeast of Apia in American Samoa.<ref name="97-98 BT"/> Over the next couple of days the system moved eastwards while gradually developing further, with the NPMOC issuing a tropical cyclone formation alert on the system early on February 1.<ref name="97-98 BT"/><ref name="VW1">{{cite web|title=Tropical Cyclone 18P (Veli) warning February 1, 1998 09z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020106.wrn |accessdate=August 5, 2012 |publisher=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/69X412j2n?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh181998.98020106.wrn |archivedate=July 30, 2012 |date=February 1, 1998 |deadurl=no |df=mdy }}</ref> Later that day the FMS named the system Veli as it had intensified into a category 1 tropical cyclone, while it came under the influence of a mid level trough of low pressure and started to move towards the southeast.<ref name="VW1"/> Later that day the NPMOC started to issue warnings on the system and designated it as Tropical Cyclone 18P, after it had continued to organize and convection surrounding the system had increased.<ref name="VW1"/> During that day Veli continued to move towards the southeast while gradually intensifying, before early the next day the NPMOC reported that the system had peaked with 1-minute sustained wind speeds of 140&nbsp;km/h (85&nbsp;mph).<ref name="18P BT">{{cite web|accessdate=August 4, 2012 |publisher=Naval Pacific Meteorology and Oceanography Center |archivedate=August 5, 2012 |title=Tropical Cyclone 18P (Katrina) best track analysis |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh181998.txt |archiveurl=http://www.webcitation.org/69g4mCGLv?url=http%3A%2F%2Fwww.usno.navy.mil%2FNOOC%2Fnmfc-ph%2FRSS%2Fjtwc%2Fbest_tracks%2F1998%2F1998s-bsh%2Fbsh181998.txt |deadurl=no |df=mdy }}</ref> Veli peaked as a category 2 tropical cyclone early on February 2, with 10-minute sustained wind speeds of 100&nbsp;km/h (65&nbsp;mph).<ref name="97-98 BT"/> Over the next day, the cyclone moved through the Tuamotu group of islands, as it began to experience significant vertical windshear and weakened into a depression.<ref name="VW6">{{cite web|title=Tropical Cyclone 18P (Veli) warning February 3, 1998 21z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020400.wrn |publisher=United States Navy, United States Air Force |accessdate=August 5, 2012 |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/69g3NrehP?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh181998.98020400.wrn |archivedate=August 4, 2012 |date=February 1, 1998 |deadurl=no |df=mdy }}</ref> The system was subsequently monitored until it was last noted during February 4, about {{Convert|1500|km|mi|disp=5|abbr=on}} to the northwest of [[Adamstown, Pitcairn Islands|Adamstown]] on the [[Pitcairn Islands]].<ref name="Wellington BT"/> In association with Tropical Cyclone Ursula, Veli brought significant waves to French Polynesia's Tuamotu province and caused minor damages on the islands of Mataiva, Rangiroa, Makatea.<ref name="GP March 1998"/> Mataiva was the worst hit island with roads and bridges washed away, and 39 homes damaged.<ref name="GP March 1998"/> On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted after coral and sand washed up onshore.<ref name="GP March 1998"/>
+During January 30, a tropical depression developed about {{convert|650|km|mi|disp=5|abbr=on}} to the northeast of Apia in American Samoa.<ref name="97-98 BT"/> Over the next couple of days the system moved eastwards while gradually developing further, with the NPMOC issuing a tropical cyclone formation alert on the system early on February 1.<ref name="97-98 BT"/><ref name="VW1">{{cite web|title=Tropical Cyclone 18P (Veli) warning February 1, 1998 09z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020106.wrn |accessdate=August 5, 2012 |publisher=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/69X412j2n?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020106.wrn |archivedate=July 30, 2012 |date=February 1, 1998 |deadurl=no |df=mdy }}</ref> Later that day the FMS named the system Veli as it had intensified into a category 1 tropical cyclone, while it came under the influence of a mid level trough of low pressure and started to move towards the southeast.<ref name="VW1"/> Later that day the NPMOC started to issue warnings on the system and designated it as Tropical Cyclone 18P, after it had continued to organize and convection surrounding the system had increased.<ref name="VW1"/> During that day Veli continued to move towards the southeast while gradually intensifying, before early the next day the NPMOC reported that the system had peaked with 1-minute sustained wind speeds of 140&nbsp;km/h (85&nbsp;mph).<ref name="18P BT">{{cite web|accessdate=August 4, 2012 |publisher=Naval Pacific Meteorology and Oceanography Center |archivedate=August 5, 2012 |title=Tropical Cyclone 18P (Katrina) best track analysis |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh181998.txt |archiveurl=http://www.webcitation.org/69g4mCGLv?url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh181998.txt |deadurl=no |df=mdy }}</ref> Veli peaked as a category 2 tropical cyclone early on February 2, with 10-minute sustained wind speeds of 100&nbsp;km/h (65&nbsp;mph).<ref name="97-98 BT"/> Over the next day, the cyclone moved through the Tuamotu group of islands, as it began to experience significant vertical windshear and weakened into a depression.<ref name="VW6">{{cite web|title=Tropical Cyclone 18P (Veli) warning February 3, 1998 21z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020400.wrn |publisher=United States Navy, United States Air Force |accessdate=August 5, 2012 |author=Naval Pacific Meteorology and Oceanography Center |archiveurl=http://www.webcitation.org/69g3NrehP?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh181998.98020400.wrn |archivedate=August 4, 2012 |date=February 1, 1998 |deadurl=no |df=mdy }}</ref> The system was subsequently monitored until it was last noted during February 4, about {{Convert|1500|km|mi|disp=5|abbr=on}} to the northwest of [[Adamstown, Pitcairn Islands|Adamstown]] on the [[Pitcairn Islands]].<ref name="Wellington BT"/> In association with Tropical Cyclone Ursula, Veli brought significant waves to French Polynesia's Tuamotu province and caused minor damages on the islands of Mataiva, Rangiroa, Makatea.<ref name="GP March 1998"/> Mataiva was the worst hit island with roads and bridges washed away, and 39 homes damaged.<ref name="GP March 1998"/> On Makatea island five houses were damaged while operations at Rangiroa's airstrip were disrupted after coral and sand washed up onshore.<ref name="GP March 1998"/>
 {{Clear}}
@@ Line 339: / Line 339: @@
 }}
-On January 31, the FMS reported that a tropical depression had developed, about {{convert|230|km|mi|disp=5|abbr=on}} to the northwest of the American Samoan island of Apia.<ref name="Feb 98"/> During that day the depression moved slowly eastwards and intensified further, before it was named Wes by the FMS, after it had developed into a Category 1 tropical cyclone during February 1.<ref name="Feb 98"/> The NPMOC subsequently designated it as Tropical Cyclone 19P and initiated advisories later that day, with peak 1-minute sustained wind speeds of 85&nbsp;km/h (50&nbsp;mph).<ref name="Feb 98"/><ref>{{cite report|type= |date=February 1, 1998 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020118.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=June 28, 2014 |title=Tropical Cyclone 19P (Wes) Warning 1 February 1, 1998 15z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6MD32A0e1?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh191998.98020118.wrn |archivedate=December 28, 2013 |deadurl=no |df=mdy }}</ref> The system subsequently continued to move eastwards and passed about {{convert|95|km|mi|disp=5|abbr=on}} to the south of the Cook Island: [[Nassau (Cook Islands)|Nassau]].<ref name="1997-98 BoM"/><ref name="Feb 98"/> During February 3, the FMS reported that the system had peaked, with 10-minute sustained wind speeds of {{Convert|90|km/h|mph|disp=5|abbr=on}} which made it a category 2 tropical cyclone on the Australian scale.<ref name="97-98 BT"/> Later that day the system subsequently started to rapidly weaken as it moved into an area of higher vertical wind shear and interacted with the westerlies.<ref>{{cite report|type= |date=February 3, 1998 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020412.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=June 29, 2014 |title=Tropical Cyclone 19P (Wes) Warning 5 February 3, 1998 15z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6QhUbKB9M?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh191998.98020412.wrn |archivedate=June 29, 2014 |deadurl=no |df=mdy }}</ref><ref>{{cite report|type= |title=Tropical Cyclone 19P (Wes) Warning 6 February 4, 1998 03z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020500.wrn |author=Naval Pacific Meteorology and Oceanography Center |date=February 4, 1998 |accessdate=June 29, 2014 |archivedate=June 29, 2014 |deadurl=no |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6QhTztmRL?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh191998.98020500.wrn |df=mdy }}</ref> The system was subsequently last noted during February 5, while located about {{Convert|400|km|mi|disp=5|abbr=on}} to the east of [[Papeete]], on the island of [[Tahiti]], [[French Polynesia]].<ref name="Feb 98"/><ref name="97-98 BT"/> The system did not directly affect any inhabited islands, while there was no damage reported on [[Suwarrow]] from the system.<ref name="1997-98 BoM"/> However, 10 people were killed on the French Polynesian island of [[Tahaa]], after two days of heavy rain associated with Wes caused a landslide during February 6.<ref name="Landslide 10">{{cite news|agency=Australian Associated Press|title=Six still missing after landslide kills ten on island|date=February 8, 1998}} {{subscription required|via=Lexis Nexis}}</ref><ref name="Landslide 2">{{cite news|date=February 8, 1998 |archivedate=June 28, 2014 |deadurl=no |title=Landslide on Tahaa, French Polynesia kills at least 10 |archiveurl=http://www.webcitation.org/6Qg2RFKEU?url=http%3A%2F%2Farchives.pireport.org%2Farchive%2F1998%2Ffebruary%2F02%252D06%252Dup.html |url=http://archives.pireport.org/archive/1998/february/02-06-up.html |agency=Radio Australia |df=mdy }}</ref>
+On January 31, the FMS reported that a tropical depression had developed, about {{convert|230|km|mi|disp=5|abbr=on}} to the northwest of the American Samoan island of Apia.<ref name="Feb 98"/> During that day the depression moved slowly eastwards and intensified further, before it was named Wes by the FMS, after it had developed into a Category 1 tropical cyclone during February 1.<ref name="Feb 98"/> The NPMOC subsequently designated it as Tropical Cyclone 19P and initiated advisories later that day, with peak 1-minute sustained wind speeds of 85&nbsp;km/h (50&nbsp;mph).<ref name="Feb 98"/><ref>{{cite report|type= |date=February 1, 1998 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020118.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=June 28, 2014 |title=Tropical Cyclone 19P (Wes) Warning 1 February 1, 1998 15z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6MD32A0e1?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020118.wrn |archivedate=December 28, 2013 |deadurl=no |df=mdy }}</ref> The system subsequently continued to move eastwards and passed about {{convert|95|km|mi|disp=5|abbr=on}} to the south of the Cook Island: [[Nassau (Cook Islands)|Nassau]].<ref name="1997-98 BoM"/><ref name="Feb 98"/> During February 3, the FMS reported that the system had peaked, with 10-minute sustained wind speeds of {{Convert|90|km/h|mph|disp=5|abbr=on}} which made it a category 2 tropical cyclone on the Australian scale.<ref name="97-98 BT"/> Later that day the system subsequently started to rapidly weaken as it moved into an area of higher vertical wind shear and interacted with the westerlies.<ref>{{cite report|type= |date=February 3, 1998 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020412.wrn |author=Naval Pacific Meteorology and Oceanography Center |accessdate=June 29, 2014 |title=Tropical Cyclone 19P (Wes) Warning 5 February 3, 1998 15z |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6QhUbKB9M?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020412.wrn |archivedate=June 29, 2014 |deadurl=no |df=mdy }}</ref><ref>{{cite report|type= |title=Tropical Cyclone 19P (Wes) Warning 6 February 4, 1998 03z |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020500.wrn |author=Naval Pacific Meteorology and Oceanography Center |date=February 4, 1998 |accessdate=June 29, 2014 |archivedate=June 29, 2014 |deadurl=no |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/6QhTztmRL?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh191998.98020500.wrn |df=mdy }}</ref> The system was subsequently last noted during February 5, while located about {{Convert|400|km|mi|disp=5|abbr=on}} to the east of [[Papeete]], on the island of [[Tahiti]], [[French Polynesia]].<ref name="Feb 98"/><ref name="97-98 BT"/> The system did not directly affect any inhabited islands, while there was no damage reported on [[Suwarrow]] from the system.<ref name="1997-98 BoM"/> However, 10 people were killed on the French Polynesian island of [[Tahaa]], after two days of heavy rain associated with Wes caused a landslide during February 6.<ref name="Landslide 10">{{cite news|agency=Australian Associated Press|title=Six still missing after landslide kills ten on island|date=February 8, 1998}} {{subscription required|via=Lexis Nexis}}</ref><ref name="Landslide 2">{{cite news|date=February 8, 1998 |archivedate=June 28, 2014 |deadurl=no |title=Landslide on Tahaa, French Polynesia kills at least 10 |archiveurl=http://www.webcitation.org/6Qg2RFKEU?url=http://archives.pireport.org/archive/1998/february/02-06-up.html |url=http://archives.pireport.org/archive/1998/february/02-06-up.html |agency=Radio Australia |df=mdy }}</ref>
 {{Clear}}
@@ Line 355: / Line 355: @@
 }}
 {{main article|Cyclone Yali}}
-The system that was too become Yali was first noted as a tropical disturbance, to the northeast of Vanuatu during March 17.<ref name="29P BT">{{cite web|accessdate=February 15, 2014|publisher=United States Navy, United States Air Force|author=Joint Typhoon Warning Center|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh291998.txt|title=Tropical Cyclone 29P (Yali) best track analysis}}</ref><ref name="TCFA Y">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 15, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/tcfas/1998/sh291998.98031900.tcf |title=Tropical Cyclone Formation Alert March 17, 1998 23z |archiveurl=http://www.webcitation.org/6NPnteJpe?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Ftcfas%2F1998%2Fsh291998.98031900.tcf |accessdate=February 15, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> During that day atmospheric convection over the disturbance's low level circulation center became better defined, before the JTWC initiated advisories and designated the system as Tropical Cyclone 29P, while the system was located about {{convert|650|km|mi|disp=5|abbr=on}} to the north-northwest of [[Port Vila]].<ref name="97-98 ATCR"/><ref name="Mar 98">{{cite web|title=Monthly Global Tropical Cyclone Summary March 1998|author=Padgett, Gary|url=http://www.australiasevereweather.com.au/cyclones/1998/summ9803.htm|year=1998|accessdate=June 27, 2011|archiveurl=https://web.archive.org/web/20110605235115/http://australiasevereweather.com/cyclones/1998/summ9802.htm|archivedate=June 5, 2011|deadurl=no}}</ref> Over the next day the system moved towards the west-southwest between [[Vanuatu]] and the [[Solomon Islands]] under the influence of the [[subtropical ridge]] of [[high pressure]] to the south of the system.<ref name="JTWC 1">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 15, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh291998.98031900.wrn |title=Tropical Cyclone 29P Warning 3 March 19, 1998 21z |archiveurl=http://www.webcitation.org/6NPnepy1X?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh291998.98031900.wrn |accessdate=February 15, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> RSMC Nadi subsequently reported late on March 19, that the system had developed into a category 1 tropical cyclone and named it Yali.<ref name="97-98 ATCR"/> After it was named Yali re-curved and started moving towards the south-southeast, as the monsoonal flow to the north of the system strengthened.<ref name="97-98 ATCR"/><ref name="Mar 98"/>
+The system that was too become Yali was first noted as a tropical disturbance, to the northeast of Vanuatu during March 17.<ref name="29P BT">{{cite web|accessdate=February 15, 2014|publisher=United States Navy, United States Air Force|author=Joint Typhoon Warning Center|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh291998.txt|title=Tropical Cyclone 29P (Yali) best track analysis}}</ref><ref name="TCFA Y">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 15, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/tcfas/1998/sh291998.98031900.tcf |title=Tropical Cyclone Formation Alert March 17, 1998 23z |archiveurl=http://www.webcitation.org/6NPnteJpe?url=http://www.nrlmry.navy.mil/atcf_web/docs/tcfas/1998/sh291998.98031900.tcf |accessdate=February 15, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> During that day atmospheric convection over the disturbance's low level circulation center became better defined, before the JTWC initiated advisories and designated the system as Tropical Cyclone 29P, while the system was located about {{convert|650|km|mi|disp=5|abbr=on}} to the north-northwest of [[Port Vila]].<ref name="97-98 ATCR"/><ref name="Mar 98">{{cite web|title=Monthly Global Tropical Cyclone Summary March 1998|author=Padgett, Gary|url=http://www.australiasevereweather.com.au/cyclones/1998/summ9803.htm|year=1998|accessdate=June 27, 2011|archiveurl=https://web.archive.org/web/20110605235115/http://australiasevereweather.com/cyclones/1998/summ9802.htm|archivedate=June 5, 2011|deadurl=no}}</ref> Over the next day the system moved towards the west-southwest between [[Vanuatu]] and the [[Solomon Islands]] under the influence of the [[subtropical ridge]] of [[high pressure]] to the south of the system.<ref name="JTWC 1">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |archivedate=February 15, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh291998.98031900.wrn |title=Tropical Cyclone 29P Warning 3 March 19, 1998 21z |archiveurl=http://www.webcitation.org/6NPnepy1X?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh291998.98031900.wrn |accessdate=February 15, 2014 |author=Joint Typhoon Warning Center |df=mdy }}</ref> RSMC Nadi subsequently reported late on March 19, that the system had developed into a category 1 tropical cyclone and named it Yali.<ref name="97-98 ATCR"/> After it was named Yali re-curved and started moving towards the south-southeast, as the monsoonal flow to the north of the system strengthened.<ref name="97-98 ATCR"/><ref name="Mar 98"/>
 For the next 2½ days, Yali moved to the southeast, passing west of the Vanuatu Islands. Yali came close enough to affect the isles of Tanna and Aneityum. Yali reached hurricane-force on the afternoon of March 21 and passed {{convert|60|nmi|km|-1}} west of Port Vila the next day.<ref name="Mar 98"/> Yali's peak intensity of {{convert|80|mi/h|km/h|-1|abbr=on}} and 965 [[millibars]] was reached on March 22 at 600 [[UTC]].<ref name="Mar 98"/> At this time, Yali was just south of [[Port Vila]], brushing it with {{convert|15|mi/h|km/h|0|abbr=on}} winds and a minimal pressure of 992 [[millibars]]. There was a possibility that the low wind reading based on poor exposure of the instrument. By 1800 [[UTC]] March 22, Yali reached its most easternmost position at {{convert|220|nmi|km|-1}} southeast of [[Port Vila]]. The upper ridge to its north intensified, increasing wind shear and limiting convection. Due to this, Yali began to weaken and dropped below hurricane force.<ref name="Mar 98"/> At around the same time, a mid-level subtropical ridge began to influence its motion, sending it to the west. As Yali moved to the southwest, the wind field became asymmetric. At 1200 [[UTC]] March 23, Yali was just east of [[Noumea, New Caledonia]] with winds of 50&nbsp;mph (80&nbsp;km/h). The weakening Yali passed just south of [[New Caledonia]] on the night of March 23. By March 25, an upper-level low had caught the cyclone and influenced the circulation with cold air.<ref name="Mar 98"/>
@@ Line 391: / Line 391: @@
 {{main article|Cyclone Alan}}
-On April 17, the FMS started to monitor a tropical disturbance, that had developed to the east of the Northern [[Cook Islands]].<ref name="97-98 ATCR"/><ref name="GP 9804"/> Over the next few days the system moved erratically, before it developed into a Category 1 tropical cyclone and was named Alan by the FMS during April 21.<ref name="97-98 ATCR"/> When it was named the system was located about {{convert|300|km|mi|disp=5|abbr=on}} to the east-southeast of Manihiki and had started to move westwards.<ref name="1997-98 BoM"/> During April 22, the FMS estimated that Alan had reached its peak intensity with 10-minute sustained wind speeds of 75&nbsp;km/h (45&nbsp;mph), as the system started to pose several forecasting challenges as it was difficult to locate and estimate how intense the system was.<ref name="1997-98 BoM"/><ref name="Wellington BT"/> Later that day the NPMOC started to issue warnings on Alan and estimated peak 1-minute sustained wind speeds of 85&nbsp;km/h (50&nbsp;mph).<ref name="April tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks April 1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9804.htm |author=Padgett, Gary |archiveurl=http://www.webcitation.org/6NEpV5uto?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Ftrak9804.htm |archivedate=February 8, 2014 |accessdate=February 8, 2014 |deadurl=no |df=mdy }}</ref><ref name="NPMOC A1">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 1 April 22, 1998 21z |archivedate=February 8, 2014 |accessdate=February 8, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042218.wrn |archiveurl=http://www.webcitation.org/6NFCBPP1l?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh321998.98042218.wrn |df=mdy }}</ref> During April 23, the system appeared to become sheared with the low level circulation centre displaced about {{convert|20|km|mi|disp=5|abbr=on}} from the nearest atmospheric convection.<ref name="1997-98 BoM"/><ref name="NPMOC 3">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 3 April 23, 1998 21z |archivedate=February 9, 2014 |accessdate=February 9, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042318.wrn |archiveurl=http://www.webcitation.org/6NGFQ1pY4?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh321998.98042318.wrn |df=mdy }}</ref> As a result, the FMS reported that Alan had weakened into a depression, while the NPMOC issued their final advisory on the system.<ref name="97-98 ATCR"/><ref name="GP 9804"/><ref name="NPMOC 3"/> Over the next day as a mid level trough of low pressure that had been shearing the system moved faster than expected the depression became better organized.<ref name="NPMOC 4"/><ref name="GP 9804"/>
+On April 17, the FMS started to monitor a tropical disturbance, that had developed to the east of the Northern [[Cook Islands]].<ref name="97-98 ATCR"/><ref name="GP 9804"/> Over the next few days the system moved erratically, before it developed into a Category 1 tropical cyclone and was named Alan by the FMS during April 21.<ref name="97-98 ATCR"/> When it was named the system was located about {{convert|300|km|mi|disp=5|abbr=on}} to the east-southeast of Manihiki and had started to move westwards.<ref name="1997-98 BoM"/> During April 22, the FMS estimated that Alan had reached its peak intensity with 10-minute sustained wind speeds of 75&nbsp;km/h (45&nbsp;mph), as the system started to pose several forecasting challenges as it was difficult to locate and estimate how intense the system was.<ref name="1997-98 BoM"/><ref name="Wellington BT"/> Later that day the NPMOC started to issue warnings on Alan and estimated peak 1-minute sustained wind speeds of 85&nbsp;km/h (50&nbsp;mph).<ref name="April tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks April 1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9804.htm |author=Padgett, Gary |archiveurl=http://www.webcitation.org/6NEpV5uto?url=http://www.australiasevereweather.com.au/cyclones/1998/trak9804.htm |archivedate=February 8, 2014 |accessdate=February 8, 2014 |deadurl=yes |df=mdy }}</ref><ref name="NPMOC A1">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 1 April 22, 1998 21z |archivedate=February 8, 2014 |accessdate=February 8, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042218.wrn |archiveurl=http://www.webcitation.org/6NFCBPP1l?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042218.wrn |df=mdy }}</ref> During April 23, the system appeared to become sheared with the low level circulation centre displaced about {{convert|20|km|mi|disp=5|abbr=on}} from the nearest atmospheric convection.<ref name="1997-98 BoM"/><ref name="NPMOC 3">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 3 April 23, 1998 21z |archivedate=February 9, 2014 |accessdate=February 9, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042318.wrn |archiveurl=http://www.webcitation.org/6NGFQ1pY4?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042318.wrn |df=mdy }}</ref> As a result, the FMS reported that Alan had weakened into a depression, while the NPMOC issued their final advisory on the system.<ref name="97-98 ATCR"/><ref name="GP 9804"/><ref name="NPMOC 3"/> Over the next day as a mid level trough of low pressure that had been shearing the system moved faster than expected the depression became better organized.<ref name="NPMOC 4"/><ref name="GP 9804"/>
-As a result, the NPMOC initiated advisories on the system again during April 24, while the FMS reported that Alan had re-intensified into a category 1 tropical cyclone later that day.<ref name="Wellington BT"/><ref name="NPMOC 4"/> The system was now located about {{convert|555|km|mi|disp=5|abbr=on}} to the west-northwest of the [[French Polynesia]]n island of [[Tahiti]], and was now moving towards the south-southeast under the influence of an upper level anticyclone located to the east of Alan.<ref name="NPMOC 4"/><ref name="GP 9804"/> Early on April 25, Alan passed near too or over the French Polynesian [[Society Islands]] of [[Maupiti]], [[Bora-Bora]], and [[Raiatea]].<ref name="GP 9804"/> During April 25, strong wind shear pulled the system apart, with visible imagery showing that the system had a fully exposed low level circulation.<ref name="97-98 ATCR"/> As a result, the FMS reported that the system had weakened into a depression at 1800&nbsp;UTC that day, while it was located about {{convert|185|km|mi|disp=5|abbr=on}} to the west-northwest of Tahiti.<ref name="97-98 ATCR"/><ref name="GP 9804"/> The NPMOC subsequently reissued their final advisory early the next day, as the system drifted towards the south-southeast while located to the west of Tahiti.<ref name="GP 9804"/><ref name="NPMOC 7">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 7 April 26, 1998 03z |date=April 26, 1998 |archivedate=February 9, 2014 |accessdate=February 9, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042600.wrn |archiveurl=http://www.webcitation.org/6NGVKvY4a?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh321998.98042600.wrn |df=mdy }}</ref> The system affected French Polynesia with high winds and torrential rain, which caused several landslides within the Society Islands.<ref name="GP 9804"/><ref name="Eight dead">{{cite news|title=At least eight killed by French Polynesia cyclone |url=http://pidp.org/archive/1998/april/04-28-01.htm |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 9, 2014 |date=April 27, 1998 |newspaper=Pacific Islands Report |archiveurl=http://www.webcitation.org/6NGhEhNlA?url=http%3A%2F%2Fpidp.org%2Farchive%2F1998%2Fapril%2F04-28-01.htm |archivedate=February 9, 2014 |deadurl=no |df=mdy }}</ref> The landslides caused two bridges to collapse and along with fallen trees blocked roads.<ref name="GP 9805"/> Overall ten people died as a result of the system while thirty others were injured, with the majority of the casualties occurring due to landslides.<ref name="1997-98 BoM"/><ref name="pidp.org">{{cite news|url=http://pidp.org/archive/1998/may/05-01-03.htm |date=May 1, 1998 |newspaper=Pacific Islands Report |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 9, 2014 |title=French Polynesia cyclone deaths rise to 10 |archiveurl=http://www.webcitation.org/6NGjkxm2E?url=http%3A%2F%2Fpidp.org%2Farchive%2F1998%2Fmay%2F05-01-03.htm |archivedate=February 9, 2014 |deadurl=no |df=mdy }}</ref> On the islands of Ra'iātea, Tahaa and Huahine several churches, schools and clinics were damaged while water and electricity supplies were cut off.<ref name="1997-98 BoM"/><ref name="GP 9805">{{cite web|accessdate=May 29, 2011 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9805.htm |title=Monthly Global Tropical Cyclone Summary May 1998 |year=1998 |archiveurl=http://www.webcitation.org/6NGlDAfFC?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Fsumm9805.htm |author=Padgett, Gary |archivedate=February 9, 2014 |deadurl=no |df=mdy }}</ref> Within the islands around 750 houses were destroyed with 430 and 150 of these occurring on Huahine and Ra'iātea respectively.<ref name="GP 9805"/>
+As a result, the NPMOC initiated advisories on the system again during April 24, while the FMS reported that Alan had re-intensified into a category 1 tropical cyclone later that day.<ref name="Wellington BT"/><ref name="NPMOC 4"/> The system was now located about {{convert|555|km|mi|disp=5|abbr=on}} to the west-northwest of the [[French Polynesia]]n island of [[Tahiti]], and was now moving towards the south-southeast under the influence of an upper level anticyclone located to the east of Alan.<ref name="NPMOC 4"/><ref name="GP 9804"/> Early on April 25, Alan passed near too or over the French Polynesian [[Society Islands]] of [[Maupiti]], [[Bora-Bora]], and [[Raiatea]].<ref name="GP 9804"/> During April 25, strong wind shear pulled the system apart, with visible imagery showing that the system had a fully exposed low level circulation.<ref name="97-98 ATCR"/> As a result, the FMS reported that the system had weakened into a depression at 1800&nbsp;UTC that day, while it was located about {{convert|185|km|mi|disp=5|abbr=on}} to the west-northwest of Tahiti.<ref name="97-98 ATCR"/><ref name="GP 9804"/> The NPMOC subsequently reissued their final advisory early the next day, as the system drifted towards the south-southeast while located to the west of Tahiti.<ref name="GP 9804"/><ref name="NPMOC 7">{{cite web|publisher=United States Navy, United States Air Force |deadurl=no |author=Naval Pacific Meteorology and Oceanography Center |title=Tropical Cyclone 32P (Alan) Warning 7 April 26, 1998 03z |date=April 26, 1998 |archivedate=February 9, 2014 |accessdate=February 9, 2014 |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042600.wrn |archiveurl=http://www.webcitation.org/6NGVKvY4a?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh321998.98042600.wrn |df=mdy }}</ref> The system affected French Polynesia with high winds and torrential rain, which caused several landslides within the Society Islands.<ref name="GP 9804"/><ref name="Eight dead">{{cite news|title=At least eight killed by French Polynesia cyclone |url=http://pidp.org/archive/1998/april/04-28-01.htm |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 9, 2014 |date=April 27, 1998 |newspaper=Pacific Islands Report |archiveurl=http://www.webcitation.org/6NGhEhNlA?url=http://pidp.org/archive/1998/april/04-28-01.htm |archivedate=February 9, 2014 |deadurl=yes |df=mdy }}</ref> The landslides caused two bridges to collapse and along with fallen trees blocked roads.<ref name="GP 9805"/> Overall ten people died as a result of the system while thirty others were injured, with the majority of the casualties occurring due to landslides.<ref name="1997-98 BoM"/><ref name="pidp.org">{{cite news|url=http://pidp.org/archive/1998/may/05-01-03.htm |date=May 1, 1998 |newspaper=Pacific Islands Report |publisher=Pacific Islands Development Program/Center for Pacific Islands Studies |accessdate=February 9, 2014 |title=French Polynesia cyclone deaths rise to 10 |archiveurl=http://www.webcitation.org/6NGjkxm2E?url=http://pidp.org/archive/1998/may/05-01-03.htm |archivedate=February 9, 2014 |deadurl=yes |df=mdy }}</ref> On the islands of Ra'iātea, Tahaa and Huahine several churches, schools and clinics were damaged while water and electricity supplies were cut off.<ref name="1997-98 BoM"/><ref name="GP 9805">{{cite web|accessdate=May 29, 2011 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9805.htm |title=Monthly Global Tropical Cyclone Summary May 1998 |year=1998 |archiveurl=http://www.webcitation.org/6NGlDAfFC?url=http://www.australiasevereweather.com.au/cyclones/1998/summ9805.htm |author=Padgett, Gary |archivedate=February 9, 2014 |deadurl=no |df=mdy }}</ref> Within the islands around 750 houses were destroyed with 430 and 150 of these occurring on Huahine and Ra'iātea respectively.<ref name="GP 9805"/>
 {{Clear}}
@@ Line 409: / Line 409: @@
 }}
-During April 28, a tropical depression developed out of an area of low pressure, about {{convert|650|km|mi|disp=5|abbr=on}} to the northeast of Papeete, French Polynesia.<ref name="97-98 ATCR"/><ref name="97-98 BT"/> Over the next 24 hours the depression moved quickly to the southeast, while gradually intensifying with nearby [[automatic weather station]]s reporting strong winds and significant pressure drops.<ref name="97-98 ATCR"/><ref name="37P BT"/> The depression was subsequently named Bart by the FMS during April 29, after it had developed into a category 1 tropical cyclone on the Australian scale near the island of [[Hao (French Polynesia)|Hao]].<ref name="GP 9804">{{cite web|accessdate=May 29, 2011 |author=Padgett, Gary |year=1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9804.htm |title=Monthly Global Tropical Cyclone Summary April 1998 |archiveurl=http://www.webcitation.org/64hvdoixL?url=http%3A%2F%2Fwww.australiasevereweather.com%2Fcyclones%2F1998%2Fsumm9804.htm |archivedate=January 15, 2012 |deadurl=no |df=mdy }}</ref><ref name="Bart1">{{cite web|author=Naval Pacific Meteorology and Oceanography Center|date=April 30, 1998|accessdate=June 5, 2011|title=Tropical Cyclone 37P (Bart) warning April 30, 1998 18z|deadurl=no|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh371998.98043018.wrn|publisher=United States Navy, United States Air Force|archivedate=June 5, 2011|archiveurl=http://www.webcitation.org/5zDMlZNhA?url=http://www.nrlmry.navy.mil/tc-bin/tc_display.cgi?STATUS%3Dinactive%26ACTION%3DLatest_Photos%26ACTIVES%3DNone%26MOSAIC_SCALE%3D20%26PHOT%3Dyes%26ATCF_BASIN%3Dsh%26BASIN%3DSHEM%26STORM_NAME%3D37P.BART%26CGI%3DSATPRODUCTS%26AGE%3DPrev%26AID_DIR%3D/SATPRODUCTS/kauai_data/www/pacific/southern_hemisphe}}</ref> The FMS reported during the next day that Bart had reached its peak 10-minute sustained windspeeds of 85&nbsp;km/h (50&nbsp;mph), as the system slowed down due to a blocking ridge of high pressure strengthening.<ref name="97-98 ATCR"/><ref name="97-98 BT"/>
+During April 28, a tropical depression developed out of an area of low pressure, about {{convert|650|km|mi|disp=5|abbr=on}} to the northeast of Papeete, French Polynesia.<ref name="97-98 ATCR"/><ref name="97-98 BT"/> Over the next 24 hours the depression moved quickly to the southeast, while gradually intensifying with nearby [[automatic weather station]]s reporting strong winds and significant pressure drops.<ref name="97-98 ATCR"/><ref name="37P BT"/> The depression was subsequently named Bart by the FMS during April 29, after it had developed into a category 1 tropical cyclone on the Australian scale near the island of [[Hao (French Polynesia)|Hao]].<ref name="GP 9804">{{cite web|accessdate=May 29, 2011 |author=Padgett, Gary |year=1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/summ9804.htm |title=Monthly Global Tropical Cyclone Summary April 1998 |archiveurl=http://www.webcitation.org/64hvdoixL?url=http://www.australiasevereweather.com/cyclones/1998/summ9804.htm |archivedate=January 15, 2012 |deadurl=no |df=mdy }}</ref><ref name="Bart1">{{cite web|author=Naval Pacific Meteorology and Oceanography Center |date=April 30, 1998 |accessdate=June 5, 2011 |title=Tropical Cyclone 37P (Bart) warning April 30, 1998 18z |deadurl=no |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh371998.98043018.wrn |publisher=United States Navy, United States Air Force |archivedate=June 5, 2011 |archiveurl=http://www.webcitation.org/5zDMlZNhA?url=http://www.nrlmry.navy.mil/tc-bin/tc_display.cgi?STATUS=inactive&ACTION=Latest_Photos&ACTIVES=None&MOSAIC_SCALE=20&PHOT=yes&ATCF_BASIN=sh&BASIN=SHEM&STORM_NAME=37P.BART&CGI=SATPRODUCTS&AGE=Prev&AID_DIR=%2FSATPRODUCTS%2Fkauai_data%2Fwww%2Fpacific%2Fsouthern_hemisphe |df= }}</ref> The FMS reported during the next day that Bart had reached its peak 10-minute sustained windspeeds of 85&nbsp;km/h (50&nbsp;mph), as the system slowed down due to a blocking ridge of high pressure strengthening.<ref name="97-98 ATCR"/><ref name="97-98 BT"/>
-The NPMOC subsequently initiated advisories on Bart and designated it as Tropical Cyclone 37P, while it was at its peak 1-minute sustained windspeeds of 65&nbsp;km/h (40&nbsp;mph).<ref name="37P BT">{{cite web|title=Tropical Cyclone 37P (Bart) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh371998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|date=December 17, 2002|publisher=United States Navy, United States Air Force|accessdate=May 29, 2011}}</ref><ref name="Bart1"/> However, by this time Bart had started to weaken, before on May 1, satellite imagery showed that the systems, low level centre had become exposed as the main area of convection had become sheared.<ref name="97-98 ATCR"/> Despite gale force wind speeds occurring in Bart's southern semicircle, the system weakened into a tropical depression during May 1, before it dissipated to the north of [[Pitcairn Island]] on May 3.<ref name="97-98 ATCR"/><ref name="GP 9804"/><ref name="Bart3">{{cite web|title=Tropical Cyclone 37P (Bart) warning May 2, 1998 06z |deadurl=no |date=April 30, 1998 |publisher=United States Navy, United States Air Force |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh371998.98050212.wrn |archiveurl=http://www.webcitation.org/64fzpNhnV?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh371998.98050212.wrn |author=Naval Pacific Meteorology and Oceanography Center |archivedate=January 14, 2012 |accessdate=June 5, 2011 |df=mdy }}</ref> Minor damage was recorded in French Polynesia, while 10 deaths were associated with Bart after waves from the system capsized a boat.<ref name="1997-98 BoM"/><ref name="97-98 ATCR"/><ref name="PDN:Bart">{{cite web|date=September 17, 2008|archiveurl=http://www.webcitation.org/64hvWw75M?url=http://www.pacificdisaster.net/pdn2008/ExportPdfServlet?header%3DEvent%20Information%26sql%3DSelect%20%2A%20From%20Event%20Where%20Id%3D174%26photo%3D|deadurl=no|publisher=Pacific Disaster.Net|title=Event Information: Tropical Cyclone Bart|author=May, Jutta|url=http://www.pacificdisaster.net/pdn2008/ExportPdfServlet?header=Event%20Information&sql=Select%20*%20From%20Event%20Where%20Id=174&photo=|accessdate=June 2, 2011|archivedate=January 15, 2012}}</ref>
+The NPMOC subsequently initiated advisories on Bart and designated it as Tropical Cyclone 37P, while it was at its peak 1-minute sustained windspeeds of 65&nbsp;km/h (40&nbsp;mph).<ref name="37P BT">{{cite web|title=Tropical Cyclone 37P (Bart) best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh371998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|date=December 17, 2002|publisher=United States Navy, United States Air Force|accessdate=May 29, 2011}}</ref><ref name="Bart1"/> However, by this time Bart had started to weaken, before on May 1, satellite imagery showed that the systems, low level centre had become exposed as the main area of convection had become sheared.<ref name="97-98 ATCR"/> Despite gale force wind speeds occurring in Bart's southern semicircle, the system weakened into a tropical depression during May 1, before it dissipated to the north of [[Pitcairn Island]] on May 3.<ref name="97-98 ATCR"/><ref name="GP 9804"/><ref name="Bart3">{{cite web|title=Tropical Cyclone 37P (Bart) warning May 2, 1998 06z |deadurl=no |date=April 30, 1998 |publisher=United States Navy, United States Air Force |url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh371998.98050212.wrn |archiveurl=http://www.webcitation.org/64fzpNhnV?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh371998.98050212.wrn |author=Naval Pacific Meteorology and Oceanography Center |archivedate=January 14, 2012 |accessdate=June 5, 2011 |df=mdy }}</ref> Minor damage was recorded in French Polynesia, while 10 deaths were associated with Bart after waves from the system capsized a boat.<ref name="1997-98 BoM"/><ref name="97-98 ATCR"/><ref name="PDN:Bart">{{cite web|date=September 17, 2008 |archiveurl=http://www.webcitation.org/64hvWw75M?url=http://www.pacificdisaster.net/pdn2008/ExportPdfServlet?header=Event%20Information&sql=Select%20%2A%20From%20Event%20Where%20Id%3D174&photo= |deadurl=no |publisher=Pacific Disaster.Net |title=Event Information: Tropical Cyclone Bart |author=May, Jutta |url=http://www.pacificdisaster.net/pdn2008/ExportPdfServlet?header=Event%20Information&sql=Select%20*%20From%20Event%20Where%20Id=174&photo= |accessdate=June 2, 2011 |archivedate=January 15, 2012 |df= }}</ref>
 {{Clear}}
 ===Other systems===
-On October 24, the United States Armed Forces started to monitor an area of disturbed weather, that was located about 800&nbsp;km (500&nbsp;mi) to the north of Nadi, Fiji.<ref name="03P">{{cite web|date=December 17, 2002|title=Tropical Cyclone 03P best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh031998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force|accessdate=June 5, 2011}}</ref> Over the next couple of days the system moved towards the southwest before early on October 26, as convection surrounding the system organized further, the FMS reported that the system had developed into a tropical depression, while the JTWC issued a tropical cyclone formation alert on it.<ref name="GP1097"/><ref name="03P W1">{{cite web|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh031998.97102612.wrn |date=October 26, 1997 |accessdate=June 30, 2011 |title=Tropical Cyclone 03P Warning 1 October 26, 1997 1500 UTC |author=Joint Typhoon Warning Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/64htFqcFf?url=http%3A%2F%2Fwww.nrlmry.navy.mil%2Fatcf_web%2Fdocs%2Fwarnings%2F1998%2Fsh031998.97102612.wrn |archivedate=January 15, 2012 |deadurl=no |df=mdy }}</ref> Later that day the JTWC initiated advisories on the depression designating it as Tropical Cyclone 03P, while it was at its peak 1-minute sustained windspeeds of 65&nbsp;km/h (40&nbsp;mph).<ref name="03P"/><ref name="03P W1"/> Over the next couple of days, a trough of low pressure approached the system and caused the depression to move south-eastwards, before the system dissipated to the north west of Fiji during October 28.<ref name="GP1097"/> On February 11, a tropical depression developed about 185&nbsp;km (115&nbsp;mi) to the northwest of the Northern Cook Island: Suwarrow Atoll.<ref name="Feb 98"/> Over the next couple of days the depression moved westwards slowly before the centre was relocated late on February 13 to a position about 185&nbsp;km (115&nbsp;mi) to the south-southeast of Nassau Island.<ref name="Feb 98"/> Over the next few days the depression remained in the same general area before the final advisory was issued on February 15.<ref name="Feb 98"/> On February 28, the FMS reported that two tropical depressions had developed within the basin.<ref name="Feb 98"/> The first depression developed about 555&nbsp;km (345&nbsp;mi) to the northwest the French Polynesian island of Tahiti, before the final warning was issued during the next day after no development had occurred.<ref name="Feb 98"/> The second depression developed about 500&nbsp;km (310&nbsp;mi) to the southeast of Honiara on the Solomon island of Guadalcanal, over the next couple of days the depression drifted towards the southeast, before the final warning was issued on March 2.<ref name="Mar 98"/>
+On October 24, the United States Armed Forces started to monitor an area of disturbed weather, that was located about 800&nbsp;km (500&nbsp;mi) to the north of Nadi, Fiji.<ref name="03P">{{cite web|date=December 17, 2002|title=Tropical Cyclone 03P best track analysis|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/best_tracks/1998/1998s-bsh/bsh031998.txt|author=Naval Pacific Meteorology and Oceanography Center, Joint Typhoon Warning Center|publisher=United States Navy, United States Air Force|accessdate=June 5, 2011}}</ref> Over the next couple of days the system moved towards the southwest before early on October 26, as convection surrounding the system organized further, the FMS reported that the system had developed into a tropical depression, while the JTWC issued a tropical cyclone formation alert on it.<ref name="GP1097"/><ref name="03P W1">{{cite web|url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh031998.97102612.wrn |date=October 26, 1997 |accessdate=June 30, 2011 |title=Tropical Cyclone 03P Warning 1 October 26, 1997 1500 UTC |author=Joint Typhoon Warning Center |publisher=United States Navy, United States Air Force |archiveurl=http://www.webcitation.org/64htFqcFf?url=http://www.nrlmry.navy.mil/atcf_web/docs/warnings/1998/sh031998.97102612.wrn |archivedate=January 15, 2012 |deadurl=no |df=mdy }}</ref> Later that day the JTWC initiated advisories on the depression designating it as Tropical Cyclone 03P, while it was at its peak 1-minute sustained windspeeds of 65&nbsp;km/h (40&nbsp;mph).<ref name="03P"/><ref name="03P W1"/> Over the next couple of days, a trough of low pressure approached the system and caused the depression to move south-eastwards, before the system dissipated to the north west of Fiji during October 28.<ref name="GP1097"/> On February 11, a tropical depression developed about 185&nbsp;km (115&nbsp;mi) to the northwest of the Northern Cook Island: Suwarrow Atoll.<ref name="Feb 98"/> Over the next couple of days the depression moved westwards slowly before the centre was relocated late on February 13 to a position about 185&nbsp;km (115&nbsp;mi) to the south-southeast of Nassau Island.<ref name="Feb 98"/> Over the next few days the depression remained in the same general area before the final advisory was issued on February 15.<ref name="Feb 98"/> On February 28, the FMS reported that two tropical depressions had developed within the basin.<ref name="Feb 98"/> The first depression developed about 555&nbsp;km (345&nbsp;mi) to the northwest the French Polynesian island of Tahiti, before the final warning was issued during the next day after no development had occurred.<ref name="Feb 98"/> The second depression developed about 500&nbsp;km (310&nbsp;mi) to the southeast of Honiara on the Solomon island of Guadalcanal, over the next couple of days the depression drifted towards the southeast, before the final warning was issued on March 2.<ref name="Mar 98"/>
 ==Season effects==
@@ Line 426: / Line 426: @@
 | {{Sort|02|03P}} || {{Sort|1026|October 26&nbsp;– 28}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical Depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|55&nbsp;km/h (35&nbsp;mph)}} || bgcolor=#{{storm colour|TD}}|{{Sort|997|997&nbsp;hPa (29.44&nbsp;inHg)}} || None || {{ntsh|0}} None || {{ntsh|0}} None ||<ref name="03P"/>
 |-
-| {{Sort|03|Martin}} || {{Sort|1031|October 27&nbsp;– November 5}} || bgcolor=#{{storm colour|A3}}|{{Sort|3|Category 3 severe tropical cyclone}} || bgcolor=#{{storm colour|A3}}|{{Sort|155|155&nbsp;km/h (100&nbsp;mph)}} || bgcolor=#{{storm colour|A3}}|{{Sort|945|945&nbsp;hPa (27.91&nbsp;inHg)}} || Cook Islands, French Polynesia || {{ntsp|17600000||$}} || {{Sort|28|28}} ||<ref name="97-98 ATCR"/><ref name="PCR:Martin">{{cite report|title=Project completion report on the cyclone emergency rehabilitation project (Loan 1588-COOSF) in the Cook Islands|date=November 29, 2000|accessdate=January 17, 2012|format=PDF|page=8|author=Asian Development Bank|url=http://www.adb.org/Documents/PCRs/COO/pcr_coo31619.pdf}}</ref><ref>{{cite web|accessdate=April 30, 2010 |date=June 20, 2007 |archivedate=August 1, 2010 |title=Coroner confirms Cyclone Martin Victims |url=http://www.cook-islands.gov.ck/view_release.php?release_id=811 |archiveurl=http://www.webcitation.org/5rfDAafDg?url=http%3A%2F%2Fwww.cook-islands.gov.ck%2Fview_release.php%3Frelease_id%3D811 |author=Cook Islands Government |deadurl=no |df=mdy }}</ref>
+| {{Sort|03|Martin}} || {{Sort|1031|October 27&nbsp;– November 5}} || bgcolor=#{{storm colour|A3}}|{{Sort|3|Category 3 severe tropical cyclone}} || bgcolor=#{{storm colour|A3}}|{{Sort|155|155&nbsp;km/h (100&nbsp;mph)}} || bgcolor=#{{storm colour|A3}}|{{Sort|945|945&nbsp;hPa (27.91&nbsp;inHg)}} || Cook Islands, French Polynesia || {{ntsp|17600000||$}} || {{Sort|28|28}} ||<ref name="97-98 ATCR"/><ref name="PCR:Martin">{{cite report|title=Project completion report on the cyclone emergency rehabilitation project (Loan 1588-COOSF) in the Cook Islands|date=November 29, 2000|accessdate=January 17, 2012|format=PDF|page=8|author=Asian Development Bank|url=http://www.adb.org/Documents/PCRs/COO/pcr_coo31619.pdf}}</ref><ref>{{cite web|accessdate=April 30, 2010 |date=June 20, 2007 |archivedate=August 1, 2010 |title=Coroner confirms Cyclone Martin Victims |url=http://www.cook-islands.gov.ck/view_release.php?release_id=811 |archiveurl=http://www.webcitation.org/5rfDAafDg?url=http://www.cook-islands.gov.ck/view_release.php?release_id=811 |author=Cook Islands Government |deadurl=no |df=mdy }}</ref>
 |-
 | {{Sort|04|Nute}} || {{Sort|1118|November 18&nbsp;– 19}} || bgcolor=#{{storm colour|A2}}|{{Sort|2|Category 2 tropical cyclone}} || bgcolor=#{{storm colour|A2}}|{{Sort|110|110&nbsp;km/h (70&nbsp;mph)}} || bgcolor=#{{storm colour|A2}}|{{Sort|975|975&nbsp;hPa (28.79&nbsp;inHg)}} || None || {{ntsh|0}} None || {{ntsh|0}} None ||<ref name="Nute TCR"/>
@@ Line 434: / Line 434: @@
 | {{Sort|06|Pam}} || {{Sort|1206|December 6&nbsp;– 10}} || bgcolor=#{{storm colour|A2}}|{{Sort|2|Category 2 tropical cyclone}} || bgcolor=#{{storm colour|A2}}|{{Sort|110|110&nbsp;km/h (70&nbsp;mph)}} || bgcolor=#{{storm colour|A2}}|{{Sort|975|975&nbsp;hPa (28.79&nbsp;inHg)}} || Cook Islands || {{ntsh|1}} Minor || {{ntsh|0}} None ||<ref name="97-98 ATCR"/>
 |-
-| {{Sort|08|Susan}} || {{Sort|1220|December 20&nbsp;– January 9}} || bgcolor=#{{storm colour|A5}}|{{Sort|5|Category 5 severe tropical cyclone}} || bgcolor=#{{storm colour|A5}}|{{Sort|230|230&nbsp;km/h (145&nbsp;mph)}} || bgcolor=#{{storm colour|A5}}|{{Sort|900|900&nbsp;hPa (26.56&nbsp;inHg)}} || Solomon Islands, Vanuatu, Fiji ||| {{ntsp|100000||$}} || {{nts|1}} ||<ref name="Susan Prem report"/><ref name="Sol">{{cite web|url=http://www.met.gov.sb/tcnames.pdf |publisher=Solomon Islands Meteorological Service |archivedate=March 9, 2013 |accessdate=November 25, 2015 |archiveurl=http://www.webcitation.org/6EzOpZVVt?url=http%3A%2F%2Fwww.met.gov.sb%2Ftcnames.pdf |date=September 13, 2009 |title=Tropical Cyclones/Depressions that passed through Solomon Islands Region |deadurl=no |df=mdy }}</ref>
+| {{Sort|08|Susan}} || {{Sort|1220|December 20&nbsp;– January 9}} || bgcolor=#{{storm colour|A5}}|{{Sort|5|Category 5 severe tropical cyclone}} || bgcolor=#{{storm colour|A5}}|{{Sort|230|230&nbsp;km/h (145&nbsp;mph)}} || bgcolor=#{{storm colour|A5}}|{{Sort|900|900&nbsp;hPa (26.56&nbsp;inHg)}} || Solomon Islands, Vanuatu, Fiji ||| {{ntsp|100000||$}} || {{nts|1}} ||<ref name="Susan Prem report"/><ref name="Sol">{{cite web|url=http://www.met.gov.sb/tcnames.pdf |publisher=Solomon Islands Meteorological Service |archivedate=March 9, 2013 |accessdate=November 25, 2015 |archiveurl=http://www.webcitation.org/6EzOpZVVt?url=http://www.met.gov.sb/tcnames.pdf |date=September 13, 2009 |title=Tropical Cyclones/Depressions that passed through Solomon Islands Region |deadurl=yes |df=mdy }}</ref>
 |-
 | {{Sort|07|Ron}} || {{Sort|0102|January 1&nbsp;– 8}} || bgcolor=#{{storm colour|A5}}|{{Sort|5|Category 5 severe tropical cyclone}} || bgcolor=#{{storm colour|A5}}|{{Sort|230|230&nbsp;km/h (145&nbsp;mph)}} || bgcolor=#{{storm colour|A5}}|{{Sort|900|900&nbsp;hPa (26.56&nbsp;inHg)}} || Samoa, Wallis and Futuna, Tonga || {{ntsh|1}} || {{ntsh|0}} None ||
 |-
-| {{Sort|09|Katrina}} || {{Sort|0507|January 7&nbsp;– 11}} || bgcolor=#{{storm colour|A3}}|{{Sort|3|Category 3 severe tropical cyclone}} || bgcolor=#{{storm colour|A3}}|{{Sort|150|150&nbsp;km/h (90&nbsp;mph)}} || bgcolor=#{{storm colour|A3}}|{{Sort|955|955&nbsp;hPa (28.20&nbsp;inHg)}} || Solomon Islands, Vanuatu || {{ntsp|8662696||$}} || {{nts|2}} ||<ref name="Impact">{{cite report|title=Economic Impact of Natural Disasters on development in the Pacific Volume 1: Research Report |accessdate=June 29, 2010 |archiveurl=http://www.webcitation.org/5noEcWKP4?url=http%3A%2F%2Fwww.pacificdisaster.net%2Fpdnadmin%2Fdata%2Foriginal%2Feconomic%2520impact%2520of%2520natural%2520disasters%2520on%2520development%2520in%2520the%2520pacific.pdf |archivedate=February 25, 2010 |year=2005 |author2=Prasad, Biman |author3=Kaloumaira, Atu |url=http://www.pacificdisaster.net/pdnadmin/data/original/economic%20impact%20of%20natural%20disasters%20on%20development%20in%20the%20pacific.pdf |author=McKenzie, Emily |pages=10–89 |deadurl=yes |df=mdy }}</ref>
+| {{Sort|09|Katrina}} || {{Sort|0507|January 7&nbsp;– 11}} || bgcolor=#{{storm colour|A3}}|{{Sort|3|Category 3 severe tropical cyclone}} || bgcolor=#{{storm colour|A3}}|{{Sort|150|150&nbsp;km/h (90&nbsp;mph)}} || bgcolor=#{{storm colour|A3}}|{{Sort|955|955&nbsp;hPa (28.20&nbsp;inHg)}} || Solomon Islands, Vanuatu || {{ntsp|8662696||$}} || {{nts|2}} ||<ref name="Impact">{{cite report|title=Economic Impact of Natural Disasters on development in the Pacific Volume 1: Research Report |accessdate=June 29, 2010 |archiveurl=http://www.webcitation.org/5noEcWKP4?url=http://www.pacificdisaster.net/pdnadmin/data/original/economic%20impact%20of%20natural%20disasters%20on%20development%20in%20the%20pacific.pdf |archivedate=February 25, 2010 |year=2005 |author2=Prasad, Biman |author3=Kaloumaira, Atu |url=http://www.pacificdisaster.net/pdnadmin/data/original/economic%20impact%20of%20natural%20disasters%20on%20development%20in%20the%20pacific.pdf |author=McKenzie, Emily |pages=10–89 |deadurl=yes |df=mdy }}</ref>
 |-
 | {{Sort|10|Tui}} || {{Sort|0125|January 25&nbsp;– 27}} || bgcolor=#{{storm colour|A1}}|{{Sort|1|Category 1 tropical cyclone}} || bgcolor=#{{storm colour|A1}}|{{Sort|075|75&nbsp;km/h (45&nbsp;mph)}} || bgcolor=#{{storm colour|A1}}|{{Sort|990|990&nbsp;hPa (29.25&nbsp;inHg)}} || Samoan islands || {{ntsp|1000000||$}} || {{nts|1}} ||<ref name="Impact"/>
@@ Line 448: / Line 448: @@
 | {{Sort|13|Wes}} || {{Sort|0131|January 31&nbsp;– February 5}} || bgcolor=#{{storm colour|A2}}|{{Sort|2|Category 2 tropical cyclone}} || bgcolor=#{{storm colour|A2}}|{{Sort|095|95&nbsp;km/h (60&nbsp;mph)}} || bgcolor=#{{storm colour|A2}}|{{Sort|985|985&nbsp;hPa (29.09&nbsp;inHg)}} || Cook Islands, French Polynesia || {{ntsh|0}} None || {{nts|10}} ||
 |-
-| {{Sort|14|Unnamed}} || {{Sort|0211|February 11&nbsp;– 15}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical Depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|065|65&nbsp;km/h (40&nbsp;mph)}} || bgcolor=#{{storm colour|TD}}|{{Sort|995|995&nbsp;hPa, (29.39&nbsp;inHg)}} || None || {{ntsh|0}} None || {{ntsh|0}} None ||<ref name="feb tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks February 1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9802.htm |author=Padgett, Gary |archiveurl=http://www.webcitation.org/69P3v7FSi?url=http%3A%2F%2Fwww.australiasevereweather.com.au%2Fcyclones%2F1998%2Ftrak9802.htm |archivedate=July 24, 2012 |deadurl=no |df=mdy }}</ref>
+| {{Sort|14|Unnamed}} || {{Sort|0211|February 11&nbsp;– 15}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical Depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|065|65&nbsp;km/h (40&nbsp;mph)}} || bgcolor=#{{storm colour|TD}}|{{Sort|995|995&nbsp;hPa, (29.39&nbsp;inHg)}} || None || {{ntsh|0}} None || {{ntsh|0}} None ||<ref name="feb tracks">{{cite web|title=Monthly Global Tropical Cyclone Tracks February 1998 |url=http://www.australiasevereweather.com.au/cyclones/1998/trak9802.htm |author=Padgett, Gary |archiveurl=http://www.webcitation.org/69P3v7FSi?url=http://www.australiasevereweather.com.au/cyclones/1998/trak9802.htm |archivedate=July 24, 2012 |deadurl=no |df=mdy }}</ref>
 |-
 | {{Sort|15|Unnamed}} || {{Sort|0228|February 28&nbsp;– March 2}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical Depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|45&nbsp;km/h (30&nbsp;mph)}} || bgcolor=#{{storm colour|TD}}|{{Sort|997|997&nbsp;hPa, (29.44&nbsp;inHg)}} || None || {{ntsh|0}} None || {{ntsh|0}} None ||<ref name="feb tracks"/>