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List of Category 5 Pacific hurricanes

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This is an old revision of this page, as edited by 100.8.154.55 (talk) at 04:38, 9 October 2016 (→Category 5 Pacific hurricanes: post-storm analysis concluded Patricia peaked at 215 mph and 872 mbar). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Tracks of all Category 5 Pacific hurricanes east of the International Dateline.

Category 5 hurricanes are tropical cyclones that reach Category 5 intensity on the Saffir-Simpson Hurricane Scale. They are by definition the strongest hurricanes that can form on planet Earth. They are rare in the eastern Pacific Ocean and generally form only once every several years. In general, Category 5s form in clusters in single years. Landfalls by such storms are rare due to the generally westerly path of tropical cyclones in the northern hemisphere.

The term "hurricane" is used for tropical cyclones in the Pacific Ocean, north of the equator and east of the international date line. A Category 5 Pacific hurricane is therefore a tropical cyclone in the north Pacific Ocean that reached Category 5 intensity east of the international dateline. Identical phenomena in the north Pacific Ocean west of the dateline are called "typhoons" or "super typhoons". Category 5 super typhoons generally happen several times per season, so cyclones of that intensity are not exceptional for that region. This difference in terminology therefore excludes storms such as Super Typhoon Paka and Super Typhoon Oliwa of 1997, and Super Typhoon Genevieve of 2014, which formed east of the dateline but did not reach Category 5 intensity until after crossing the dateline.

Statistics

Saffir–Simpson scale
TD TS C1 C2 C3 C4 C5

A Category 5 hurricane is defined as having sustained windspeeds of at least 137 knots (158 mph; 254 km/h) over a one-minute period 10 metres (33 ft)* above the ground.[1][2] As a tropical cyclone is moving, its wind field is asymmetric. In the northern hemisphere, the strongest winds are on the right side of the storm (relative to the direction of motion). The highest winds given in advisories are those from the right side.[3]

Since the 1959 season, only 15 hurricanes are known to have reached Category 5 intensity. There are no known Category 5 storms occurring before 1959. It is possible that some earlier storms reached Category 5 over open waters, but they were never recognized because they never affected land and remained at sea.[4]

Category 5 Pacific hurricanes

Hurricane Linda at its peak intensity on September 12, 1997.
Hurricane Patricia shortly after its record peak intensity on October 23, 2015.

This lists all of the Category 5 hurricanes in the order in which they formed. Only 1994's Hurricane Emilia and 2006's Hurricane Ioke have reached Category 5 intensity more than once; that is, by weakening into a Category 4 or weaker storm and later re-strengthening to a Category 5 storm.

Before the advent of reliable geostationary satellite coverage in 1966, the number of eastern Pacific tropical cyclones was significantly underestimated.[5] It is therefore very possible that there are additional Category 5 hurricanes other than those listed, but they were not reported and therefore not recognized. However, the lack of Pacific Category 5 hurricanes during the late 1970s, 1980s, and early 1990s, is certain.[4]

The minimum central pressure of these storms is, for the most part, estimated from satellite imagery using the Dvorak technique. In the case of Kenna,[6] Ava,[7] and Patricia, the central pressure was measured by hurricane hunter aircraft flying into the storm.[4] Because of the estimation of central pressures, it is possible that other storms more intense than these have formed.[8]

The reason for estimating the pressure (in lieu of direct measurements) is the fact that most of these storms did not threaten land.[9] As Kenna and Patricia were threatening land, their pressures were measured by Hurricane Hunters using dropsondes.[6] While Hurricane Ava never threatened land,[4] it too was flown into by Hurricane Hunters to test equipment and conduct research.[7]

Older storms have incomplete pressure readings, since there were no satellite-based estimates; the only observations were taken by ships, land-based observations, or reconnaissance aircraft when available. Ava's minimum known pressure was measured when it was a Category 4 hurricane, for example.[4] John and Gilma have incomplete pressures because the Central Pacific Hurricane Center, in general, did not publish pressure on systems in the central Pacific (140°W to the dateline) at the time.[10] However, it should be noted that this list is not identical to the list of most intense Pacific hurricanes. The most intense known Category 4 storm in the eastern Pacific was 2014's Odile. The lowest pressure of this storm was 918 millibars, lower than that of some Category 5's, such as Guillermo.[4]

Hurricanes have reached Category 5 intensity during every month from June to October. The earliest Category 5 to form in a season is 1973's Hurricane Ava, which formed on June 7. The latest Category 5 to form in a season is Hurricane Kenna, which reached peak intensity on October 24. Hurricanes Ava, Gilma, Ioke, Linda, and Patricia are the most intense storms to form in their respective months. There have been no May, November, or off-season Category 5 hurricanes.[4]

Two Pacific hurricanes are known to have reached Category 5 intensity multiple times: Emilia and Ioke. Both did it twice, and Ioke reached Category 5 status a third time as a typhoon while in the western Pacific.[4] Hurricane Ioke was tied for the longest-lasting Category 5 hurricane recorded, spending 42 hours at that strength,[11] while hurricanes John and Linda had the longest time spent consecutively at that intensity.[4]

Hurricane Hernan off the coast of Mexico on September 1, 2002, at peak strength.
Microwave radar in the tail of a C130 during a flight into Hurricane Ava.
List of Category 5 Pacific hurricanes[4]
Storm
name 		Season Dates as a
Category 5 		Time as a
Category 5 (hours) 		Peak one-minute
sustained winds 		Pressure
mph km/h hPa inHg
Patsy 1959 September 6 6 175 280 Unknown
Ava 1973 June 7 24 160 260 915 27.02
Emilia 1994 July 19–21† 18 160 260 926 27.34
Gilma 1994 July 24–25 18 160 260 920 27.17
John 1994 August 22–24 42 175 280 929 27.43
Guillermo 1997 August 4–5 24 160 260 919 27.14
Linda 1997 September 12–14 42 185 295 902 26.64
Elida 2002 July 25 6 160 260 921 27.20
Hernan 2002 September 1 12 160 260 921 27.20
Kenna 2002 October 24 18 165 270 913 26.96
Ioke 2006 August 24–26‡ 42 160 260 915 27.02
Rick 2009 October 18 24 180 285 906 26.75
Celia 2010 June 25 12 160 260 921 27.20
Marie 2014 August 24 6 160 260 918 27.11
Patricia 2015 October 22–23 24 215 345 872 25.75
† For its first time as a Category 5, Emilia was at that intensity for 6 hours; the second time was for 12 for a total of 18 hours.[12]

‡ For its first time as a Category 5, Ioke was at that intensity for 18 hours; the second time was 24 additional hours east of the dateline, giving a total of 42 hours.[4] Ioke did not lose Category 5 status on August 26, however, it moved into the Western North Pacific, and thus was no longer considered a hurricane, but rather a typhoon.

Climatology

Hurricane Guillermo, the first of two Category 5s during the 1997 season.

In the eastern Pacific, Category 5 hurricanes usually occur only in El Niño years. During El Niño years, conditions are more favorable for tropical cyclones because of warmer sea surface temperatures and reduced wind shear. This is why Category 5s cluster in single seasons. The effects of El Niño are most significant in the central Pacific (140°W to the dateline).[13]

The general lack of Category 5s in non warm-ENSO years is because of there being limited space for development. The prevailing ocean currents of the area carry warm water to the west. As there is no large piece of land to block the water and cause it to "pile up" like in the Atlantic, the area suitable for all tropical cyclones is small. Farther out to sea, while waters are still warm, wind shear limits the development of tropical cyclones in the waters south of Hawaii. This makes an otherwise ideal region unfavorable for tropical cyclones.

This does not mean that a Category 5 hurricane cannot form outside of an El Niño event. The entire year of 1959 was neither an El Niño or a La Niña, but it had one Category 5 hurricane (Patsy). Most of 1973 was during a La Niña, which reduces tropical cyclone activity in the eastern Pacific, yet Hurricane Ava, a Category 5 hurricane, formed in June of that year.[14] The 2009, 2010, 2014, and 2015 seasons are the only pairs of seasons in which a Category 5 hurricane formed in consecutive years (Rick and Celia, and Marie and Patricia, respectively).[15]

Landfalls

Hurricane Kenna, one of only three Category 5 Pacific hurricanes to make landfall at any intensity.

Of all of the Category 5 Pacific hurricanes, the only ones to make landfall at any intensity were Hurricane Kenna, Hurricane Rick, and Hurricane Patricia. None made landfall as Category 5 hurricanes; Patricia and Kenna had weakened to Category 4 at the time of their landfalls, and Rick was a tropical storm at its landfall. Patricia was the strongest landfall among Pacific hurricanes; 1976's Hurricane Madeline and 1992's Hurricane Iniki are tied as the second strongest storms at landfall, both of which didn't reach Category 5 strength, but made landfall as stronger Category 4 storms than Kenna.[6] Originally, a hurricane in 1959 was thought to have struck Manzanillo at Category 5 intensity, but a reanalysis in 2016 indicated the storm had peaked as a Category 4 hurricane, and made landfall with the same winds as Kenna.[16] Patricia was also originally thought to have made landfall as a Category 5 hurricane near Manzanillo before post-season analysis in 2016.

In addition to these three systems, Hurricanes John, Linda, and Ioke all threatened land for a while. John and Ioke had minimal impact on Johnston Atoll and John caused heavy surf in Hawaii.[12] Linda was briefly forecast to approach southern California, and it passed close to Socorro Island near peak intensity.[11][17]

The reason for the lack of landfalls is that tropical cyclones in the northern hemisphere usually travel to the west.[18] In the Atlantic, this sends hurricanes towards North America. In the eastern Pacific, this sends tropical cyclones out into the open ocean to dissipate over waters too cool to support them or in environments with high wind shear. Hawaii, the only heavily populated island chain in the eastern Pacific, is protected from most hurricanes by a subtropical ridge and is small enough to avoid being hit simply due to low odds.

See also

Template:Wikipedia books

References

  1. ^ "The Saffir-Simpson Hurricane Scale". National Hurricane Center. 2007-08-17. Retrieved 2008-09-14.
  2. ^ Chris Landsea. "Subject: D4) What does "maximum sustained wind" mean ? How does it relate to gusts in tropical cyclones?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2006-01-04.
  3. ^ Chris Landsea. "Subject: D4) What does "maximum sustained wind" mean ? How does it relate to gusts in tropical cyclones?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2006-01-04.
  4. ^ a b c d e f g h i j k "Eastern North Pacific Tracks File 1949-2007". National Hurricane Center. 2008-03-21. Archived from the original (plaintext) on 2008-08-22. Retrieved 2008-09-14.
  5. ^ Chris Landsea (2002-06-11). "Subject: E10) What are the average, most, and least tropical cyclones occurring in each basin?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2006-01-04.
  6. ^ a b c James Franklin (2002-12-26). "Tropical Cyclone Report Hurricane Kenna". National Hurricane Center. Retrieved 2008-09-14.
  7. ^ a b F.J. Hoelzl (1973-06-06). "wea01151, NOAA's National Weather Service (NWS) Collection". NOAA Photo Library. National Oceanic and Atmospheric Administration. Retrieved 2008-09-14.
  8. ^ Max Mayfield (1997-10-02). "Preliminary Report Hurricane Guillermo". National Hurricane Center. Retrieved 2008-09-16.
  9. ^ Neal Dorst. "Subject: H2) Who are the "Hurricane Hunters" and what are they looking for?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2006-01-04.
  10. ^ Jim Gross (1989-08-30). "Preliminary Report Hurricane Dalilia" (GIF). National Hurricane Center. p. 3. Retrieved 2006-01-04.
  11. ^ a b Andy Nash; Tim Craig; Sam Houston; Roy Matsuda; Jeff Powell; Ray Tanabe; Jim Weyman. "2006 Tropical Cyclones Central North Pacific". Central Pacific Hurricane Center. Retrieved 2008-09-14. {{cite web}}: Unknown parameter |last-author-amp= ignored (|name-list-style= suggested) (help)
  12. ^ a b "The 1994 Central Pacific Tropical Cyclone Season". Central Pacific Hurricane Center. Retrieved 2008-09-14.
  13. ^ Chris Landsea. "Subject: G2) How does El Niño-Southern Oscillation affect tropical cyclone activity around the globe?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2006-01-04.
  14. ^ "Cold and Warm Episodes by Season". Climate Prediction Center. Retrieved 2006-01-04.
  15. ^ National Hurricane Center; Hurricane Research Division; Central Pacific Hurricane Center (April 26, 2024). "The Northeast and North Central Pacific hurricane database 1949–2023". United States National Oceanic and Atmospheric Administration's National Weather Service. Archived from the original on May 29, 2024. A guide on how to read the database is available here. Public Domain This article incorporates text from this source, which is in the public domain.
  16. ^ Re-analysis of the 1959 Manzanillo Mexico Hurricane (PDF) (Report). National Hurricane Center. 2016-02-04. Retrieved 2016-02-04.
  17. ^ Max Mayfield (1997-10-25). "Preliminary Report Hurricane Linda". National Hurricane Center. Retrieved 2006-01-04.
  18. ^ Chris Landsea. "Subject: G8) Why do hurricanes hit the East coast of the U.S., but never the West coast?". FAQ: Hurricane, Typhoons, and Tropical Cyclones. Atlantic Oceanographic and Meteorological Laboratory Hurricane Research Division. Retrieved 2008-09-14.
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