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| Hurricane season=[[2006 Atlantic hurricane season]]
| Hurricane season=[[2006 Atlantic hurricane season]]
}}
}}
'''Tropical Storm Alberto''' was the first [[tropical cyclone|tropical storm]] of the [[2006 Atlantic hurricane season]]. Forming on June 10 in the northwestern [[Caribbean Sea]], the storm moved generally to the north, reaching a peak intensity of 70 mph (110 km/h) before weakening and moving ashore in the [[Big Bend (Florida)|Big Bend]] area of [[Florida]] on June 13. Alberto then moved through eastern [[Georgia (U.S. state)|Georgia]], [[North Carolina]], and [[Virginia]] as a [[Tropical cyclone#Intensity classifications|tropical depression]] before becoming [[extratropical]] on June 14.
'''Tropical Storm Alberto''' was the first [[tropical cyclone|tropical storm]] of the [[2006 Atlantic hurricane season]]. Forming on June 10 in the northwestern [[Caribbean Sea]], the storm moved generally to the north, reaching a maximum intensity of 70 mph (110 km/h) before weakening and moving ashore in the [[Big Bend (Florida)|Big Bend]] area of [[Florida]] on June 13. Alberto then moved through eastern [[Georgia (U.S. state)|Georgia]], [[North Carolina]], and [[Virginia]] as a [[Tropical cyclone#Intensity classifications|tropical depression]] before becoming [[extratropical]] on June 14.


Across the western Caribbean, the storm produced heavy rainfall, causing some minor damage. In Florida, a moderate [[storm tide]] caused coastal damage and flooding, while Alberto's outer rainbands produced several tornadoes. The storm was indirectly responsible for two drownings off the coast of [[Tampa Bay]]. In [[North Carolina]], heavy rainfall caused locally severe flooding, and one person drowned after running into a flooded storm drain near [[Raleigh, North Carolina|Raleigh]]. The remnants of Alberto produced strong winds and left four people missing in [[Atlantic Canada]]. Overall, damage was minor along Alberto's path.
Across the western Caribbean, the storm produced heavy rainfall, causing some minor damage. In Florida, a moderate [[storm tide]] caused coastal damage and flooding, while Alberto's outer rainbands produced several tornadoes. The storm was indirectly responsible for two drownings off the coast of [[Tampa Bay]]. In [[North Carolina]], heavy rainfall caused locally severe flooding, and one person drowned after running into a flooded storm drain near [[Raleigh, North Carolina|Raleigh]]. The remnants of Alberto produced strong winds and left four people missing in [[Atlantic Canada]]. Overall, damage was minor along Alberto's path.
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==Storm history==
==Storm history==
{{storm path|Alberto_2006_track.png}}
{{storm path|Alberto_2006_track.png}}
In early June&nbsp;2006, an area of [[atmospheric convection|convection]] persisted across [[Central America]] and the western [[Caribbean Sea]], in association with a broad, nearly stationary [[trough (meteorology)|trough]] of [[low pressure area|low pressure]].<ref name="tcr">{{cite web|author=Lixion Avila & Daniel Brown|year=2006|title=Tropical Storm Alberto Tropical Cyclone Report|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/pdf/TCR-AL012006_Alberto.pdf|format=PDF}}</ref><ref name="66two">{{cite web|author=Pasch|year=2006|title=June 6 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060608.ABNT20}}</ref> Thunderstorms increased and became more concentrated on [[June 8]] after a [[tropical wave]] moved into the western Caribbean,<ref name="tcr"/> and an upper-level low to its west increased [[outflow (meteorology)|outflow]] over the system.<ref name="rain">{{cite web|author=David Roth|year=2006|title=Tropical Storm Alberto - June 2006|publisher=Hydrometeorological Prediction Center|accessdate=2007-05-10|url=http://www.hpc.ncep.noaa.gov/tropical/rain/alberto2006.html}}</ref> It moved slowly north-northwestward, and [[tropical cyclogenesis|development]] was initially inhibited by marginally favorable upper-level winds and land interaction.<ref name="68two">{{cite web|author=Stewart|year=2006|title=June 8 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060815.ABNT20}}</ref> The system gradually organized,<ref name="69two">{{cite web|author=Mainelli/Knabb|year=2006|title=June 9 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060915.ABNT20}}</ref> and by [[June 10]] a circulation formed with sufficiently organized convection for the [[National Hurricane Center]] to classify it Tropical Depression One. At this point the storm was located about 140&nbsp;miles (225&nbsp;km) south of the western tip of [[Cuba]].<ref name="tcr"/>
In early June&nbsp;2006, an area of [[atmospheric convection|convection]] persisted across [[Central America]] and the western [[Caribbean Sea]], in association with a broad, nearly stationary [[trough (meteorology)|trough]] of [[low pressure area|low pressure]].<ref name="tcr">{{cite web|author=Lixion Avila & Daniel Brown|year=2006|title=Tropical Storm Alberto Tropical Cyclone Report|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/pdf/TCR-AL012006_Alberto.pdf|format=PDF}}</ref><ref name="66two">{{cite web|author=Pasch|year=2006|title=June 6 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060608.ABNT20}}</ref> Thunderstorms increased and became more concentrated on [[June 8]] after a [[tropical wave]] moved into the western Caribbean,<ref name="tcr"/> and an upper-level low to its west increased [[outflow (meteorology)|outflow]] over the system.<ref name="rain">{{cite web|author=David Roth|year=2006|title=Tropical Storm Alberto - June 2006|publisher=Hydrometeorological Prediction Center|accessdate=2007-05-10|url=http://www.hpc.ncep.noaa.gov/tropical/rain/alberto2006.html}}</ref> The disturbance moved slowly north-northwestward, and [[tropical cyclogenesis|development]] was initially inhibited by marginally favorable upper-level winds and land interaction.<ref name="68two">{{cite web|author=Stewart|year=2006|title=June 8 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060815.ABNT20}}</ref> The system gradually [[tropical cyclogenesis|organized]],<ref name="69two">{{cite web|author=Mainelli/Knabb|year=2006|title=June 9 Tropical Weather Outlook|publisher=National Hurricane Center|accessdate=2007-05-10|url=ftp://ftp.met.fsu.edu/pub/weather/tropical/Outlook-A/2006060915.ABNT20}}</ref> and by [[June 10]] a circulation formed with sufficiently organized convection for the [[National Hurricane Center]] to classify it Tropical Depression One. At this point the storm was located about 140&nbsp;miles (225&nbsp;km) south of the western tip of [[Cuba]].<ref name="tcr"/>


The depression tracked to the northwest through the [[Yucatán Channel]] into an area of increased [[wind shear]], which the center exposed and elongated.<ref name="tcr"/><ref name="disc1">{{cite web|author=Beven|year=2006|title=Tropical Depression One Special Discussion One|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.001.shtml?}}</ref> Despite its poor structure, the system maintained strong winds in its eastern semicircle. Based on [[Hurricane Hunters]]' reports of flight level winds of 50&nbsp;mph (80&nbsp;km/h) in a few [[rainbands|convective bands]], it is estimated the depression strengthened into a [[tropical storm]] early on [[June 11]], while located about 260&nbsp;miles (420&nbsp;km) southwest of the [[Dry Tortugas]]. The winds were not considered indicative of its intensity, which delayed the upgrade in classification for several hours, but once the upgrade took place, the [[National Hurricane Center]] designated the storm with the name Alberto.<ref name="tcr"/> Upon becoming a tropical storm, the low-level circulation had become better defined, though forecasts predicted the wind shear would increase, preventing significant strengthening of the storm.<ref name="disc6">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Six|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.006.shtml?}}</ref> One forecaster at the National Hurricane Center remarked the system resembled a [[subtropical cyclone]].<ref name="disc7">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Seven|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.007.shtml?}}</ref> However, deep convection developed and built westward against the wind shear as the overall organization improved, and at the same time Alberto turned northeastward under the influence of an approaching trough.<ref name="disc9">{{cite web|author=Franklin|year=2006|title=Tropical Storm Alberto Discussion Nine|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.009.shtml?}}</ref> On [[June 12]], the circulation abruptly reformed under the area of deepest convection, which coincided with the storm's passage over the [[loop current]]; consequentially, Alberto quickly strengthened to reach peak winds of 70&nbsp;mph (115&nbsp;km/h) about 220&nbsp;miles (350&nbsp;km) west-northwest of [[Tampa, Florida]].<ref name="tcr"/>
The depression tracked to the northwest through the [[Yucatán Channel]] into an area of increased [[wind shear]], which the center exposed and elongated.<ref name="tcr"/><ref name="disc1">{{cite web|author=Beven|year=2006|title=Tropical Depression One Special Discussion One|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.001.shtml?}}</ref> Despite its poor structure, the system maintained strong winds in its eastern semicircle. The depression intensified into Tropical Storm Alberto early on [[June 11]] about 260&nbsp;miles (420&nbsp;km) southwest of the [[Dry Tortugas]], based on [[Hurricane Hunters]]' reports of flight level winds of 50&nbsp;mph (80&nbsp;km/h) in a few [[rainbands|convective bands]].<ref name="tcr"/> Upon becoming a tropical storm, the low-level circulation had become better defined, though forecasts predicted the wind shear would increase, preventing significant strengthening of the storm.<ref name="disc6">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Six|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.006.shtml?}}</ref> One forecaster at the National Hurricane Center remarked the system resembled a [[subtropical cyclone]].<ref name="disc7">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Seven|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.007.shtml?}}</ref> However, deep convection developed and built westward against the wind shear as the overall organization improved. At the same time Alberto turned northeastward under the influence of an approaching trough.<ref name="disc9">{{cite web|author=Franklin|year=2006|title=Tropical Storm Alberto Discussion Nine|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.009.shtml?}}</ref> On [[June 12]], the circulation abruptly reformed under the area of deepest convection, which coincided with the storm's passage over the [[loop current]]; consequentially, Alberto quickly strengthened to reach peak winds of 70&nbsp;mph (115&nbsp;km/h) about 220&nbsp;miles (350&nbsp;km) west-northwest of [[Tampa, Florida]].<ref name="tcr"/>


Though it was projected to track over cooler waters and stay in an area of increased shear, forecasters at the National Hurricane Center predicted Alberto to attain hurricane status and make landfall at that intensity.<ref name="disc10">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Ten|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.010.shtml?}}</ref> The storm maintained peak intensity for about 18&nbsp;hours,<ref name="tcr"/> and while accelerating northeastward, Alberto's convection diminished as the cloud pattern became elongated.<ref name="disc11">{{Cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Eleven|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.011.shtml?}}</ref> On [[June 13]], dry air became entrained in the circulation, leaving the center exposed from the convection and the [[Radius of maximum wind|wind field]] greatly broadened.<ref name="disc13">{{cite web|author=Franklin|year=2006|title=Tropical Storm Alberto Discussion Thirteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.013.shtml?}}</ref> A partial [[eye (cyclone)|eyewall]] developed in the western semicircle of the center; however, winds were well below hurricane force.<ref name="disc14">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Fourteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.014.shtml?}}</ref> Alberto continued to weaken, and made [[landfall (meteorology)|landfall]] at about 1630 UTC on [[June 13]] with 45&nbsp;mph (75&nbsp;km/h) winds in [[Taylor County, Florida]], about 50&nbsp;miles (80&nbsp;km) [[southeast]] of [[Tallahassee, Florida|Tallahassee]].<ref name="tcr"/>
Though it was projected to track over cooler waters and stay in an area of increased shear, forecasters at the National Hurricane Center predicted Alberto to attain hurricane status and make landfall at that intensity.<ref name="disc10">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Ten|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.010.shtml?}}</ref> The storm maintained peak intensity for about 18&nbsp;hours,<ref name="tcr"/> and while accelerating northeastward, Alberto's convection diminished as the cloud pattern became elongated.<ref name="disc11">{{Cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Eleven|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.011.shtml?}}</ref> On [[June 13]], dry air became entrained in the circulation, leaving the center exposed from the convection and the [[Radius of maximum wind|wind field]] greatly broadened.<ref name="disc13">{{cite web|author=Franklin|year=2006|title=Tropical Storm Alberto Discussion Thirteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.013.shtml?}}</ref> A partial [[eye (cyclone)|eyewall]] developed in the western semicircle of the center; however, winds were well below hurricane force.<ref name="disc14">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Fourteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.014.shtml?}}</ref> Alberto continued to weaken, and made [[landfall (meteorology)|landfall]] at about 1630 UTC on [[June 13]] with 45&nbsp;mph (75&nbsp;km/h) winds in [[Taylor County, Florida]], about 50&nbsp;miles (80&nbsp;km) [[southeast]] of [[Tallahassee, Florida|Tallahassee]].<ref name="tcr"/>


[[Image:Alberto2006RadarSC.png|200px|thumb|right|Tropical Storm Alberto over South Carolina]]
[[Image:Alberto2006RadarSC.png|200px|thumb|right|Tropical Storm Alberto over South Carolina]]
The storm maintained a well-organized structure<ref name="disc15">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Fifteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.015.shtml?}}</ref> and persistent banding features over land,<ref name="disc16">{{cite web|author=Stewart|year=2006|title=Tropical Storm Alberto Discussion Sixteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.016.shtml?}}</ref> and Alberto continued to produce winds of tropical storm force as it moved into [[Georgia (U.S. state)|Georgia]]. Early on [[June 14]], the storm weakened to tropical depression status while located near the city of [[Millen, Georgia]]. Alberto began to lose tropical characteristics soon thereafter, and about six hours after weakening to a tropical depression it transitioned into an [[extratropical cyclone]].<ref name="tcr"/> Late on [[June 14]] it accelerated northeastward to emerge into the [[Atlantic Ocean]],<ref name="hpc19">{{cite web|author=Fries & Petersen|year=2006|title=Public Advisory 19 on Remnants of Alberto|publisher=Hydrometeorological Prediction Center|accessdate=2007-05-10|url=http://www.hpc.ncep.noaa.gov/tropical2006/ALBERTO/ALBERTO_19.html}}</ref> and on [[June 15]], it entered the area of responsibility of the [[Canadian Hurricane Centre]].<ref name="chc">{{cite web|author=Canadian Hurricane Center|year=2007|title=2006 Tropical Cyclone Season Summary|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/storm06.html}}</ref> While over open waters, Alberto's remnants began to re-intensify; later that day, the extratropical remnant low attained winds of 65&nbsp;mph (105&nbsp;km/h) and a pressure of 969&nbsp;[[mbar]] while a short distance south of [[Nova Scotia]].<ref name="tcr"/> At this time, the low presented a well-defined comma structure.<ref name="chc6152">{{cite web|author=Bowyer & Roussel|year=2006|title=Tropical Storm Alberto Information Statement for June 15, 2006 (2)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615235119.Alberto.txt.en}}</ref> After passing near [[Sable Island]],<ref name="chc6152"/> the remnants of Alberto crossed the [[Avalon Peninsula]] of [[Newfoundland (island)|Newfoundland]] on [[June 16]].<ref name="chc616">{{cite web|author=Roussel & Marshall|year=2006|title=Tropical Storm Alberto Information Statement for June 16, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060616115244.Alberto.txt.en}}</ref> The extratropical storm turned to the east-northeast and later to the east as it continued its rapid forward motion, and on [[June 19]] the remnants of Alberto merged with an approaching [[cold front]] near the [[British Isles]].<ref name="tcr"/>
The storm maintained a well-organized structure<ref name="disc15">{{cite web|author=Pasch|year=2006|title=Tropical Storm Alberto Discussion Fifteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.015.shtml?}}</ref> and [[tropical cyclone#banding|banding features]] over land,<ref name="disc16">{{cite web|author=Stewart|year=2006|title=Tropical Storm Alberto Discussion Sixteen|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.discus.016.shtml?}}</ref> and Alberto continued to produce winds of tropical storm force as it moved into [[Georgia (U.S. state)|Georgia]]. Early on [[June 14]], the storm weakened to tropical depression status while located near the city of [[Millen, Georgia]]. Alberto began to lose tropical characteristics soon thereafter, and about six hours after weakening to a tropical depression it transitioned into an [[extratropical cyclone]].<ref name="tcr"/> Late on [[June 14]] it accelerated northeastward to emerge into the [[Atlantic Ocean]],<ref name="hpc19">{{cite web|author=Fries & Petersen|year=2006|title=Public Advisory 19 on Remnants of Alberto|publisher=Hydrometeorological Prediction Center|accessdate=2007-05-10|url=http://www.hpc.ncep.noaa.gov/tropical2006/ALBERTO/ALBERTO_19.html}}</ref> and on [[June 15]], it entered the area of responsibility of the [[Canadian Hurricane Centre]].<ref name="chc">{{cite web|author=Canadian Hurricane Center|year=2007|title=2006 Tropical Cyclone Season Summary|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/storm06.html}}</ref> While over open waters, Alberto's remnants began to re-intensify; later that day, the extratropical remnant low attained winds of 65&nbsp;mph (105&nbsp;km/h) and a pressure of 969&nbsp;[[mbar]] while a short distance south of [[Nova Scotia]].<ref name="tcr"/> At this time, the low presented a well-defined comma structure.<ref name="chc6152">{{cite web|author=Bowyer & Roussel|year=2006|title=Tropical Storm Alberto Information Statement for June 15, 2006 (2)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615235119.Alberto.txt.en}}</ref> After passing near [[Sable Island]],<ref name="chc6152"/> the remnants of Alberto crossed the [[Avalon Peninsula]] of [[Newfoundland (island)|Newfoundland]] on [[June 16]].<ref name="chc616">{{cite web|author=Roussel & Marshall|year=2006|title=Tropical Storm Alberto Information Statement for June 16, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060616115244.Alberto.txt.en}}</ref> The extratropical storm turned to the east-northeast and later to the east as it continued its rapid forward motion, and on [[June 19]] the remnants of Alberto merged with an approaching [[cold front]] near the [[British Isles]].<ref name="tcr"/>


==Preparations==
==Preparations==
[[Image:alberto-radar-landfall.png|thumb|right|Radar image of Tropical Storm Alberto at landfall]]
[[Image:alberto-radar-landfall.png|thumb|right|Radar image of Tropical Storm Alberto at landfall]]
The Cuban government evacuated over 27,000&nbsp;people in the western portion of the country due to the threat of flooding.<ref name="cubeff">{{cite web|author=Shannon D. Harrington|year=2006|title=Alberto Heads to Florida, May Strengthen to Hurricane|publisher=Bloomberg.com|accessdate=2006-06-12|url=http://www.bloomberg.com/apps/news?pid=10000103&sid=aLHgNAaDtExY&refer=us}}</ref> The National Hurricane Center recommended [[Tropical cyclone warnings and watches#Tropical Storm Warning|tropical storm warnings]] for the [[Isle of Youth]] and the [[Pinar del Rio]] province early on [[June 10]], but they were not issued by the Cuban government.<ref name="pa2"/>
By [[June 12]], the Cuban government had evacuated over 25,000&nbsp;people in the western portion of the country due to the threat of flooding.<ref name="ips615">{{cite news|author=Dalia Acosta|date=2006-06-15|title=Tempestade tropical Alberto causa estragos; Cuba: Os estragos causados por Alberto|publisher=Inter Press Service|accessdate=2008-02-12|language=Portuguese}}</ref><ref name="afp612">{{cite web|author=Agence France-Presse|date=2006-06-12|title=25,000 Cubans move from 'life-threatening' storm Alberto|accessdate=2008-02-12|url=http://www.turkishpress.com/news.asp?id=128058}}</ref> The National Hurricane Center recommended [[Tropical cyclone warnings and watches#Tropical Storm Warning|tropical storm warnings]] for the [[Isle of Youth]] and the [[Pinar del Rio]] province early on [[June 10]], but they were not issued by the Cuban government.<ref name="pa2"/>


In northwestern Florida, officials issued a mandatory evacuation order for about 21,000&nbsp;citizens in [[Levy County, Florida|Levy County]], [[Citrus County, Florida|Citrus County]], and [[Taylor County, Florida|Taylor County]].<ref>{{cite news|url=http://abclocal.go.com/wpvi/story?section=weather&id=4261181&pt=print|title=20,000 ordered to leave Florida's Gulf Coast|publisher=[[Associated Press]]|date=[[June 12]], [[2006]]|accessdate=2006-06-13}}</ref> Several schools were closed as well, and converted into shelters.<ref>{{cite news|url=http://www.tampabays10.com/news/local/article.aspx?storyid=33249|title=Hernando County issues a recommended evacuation of Zone A/B|publisher=[[WTSP]]|date=[[June 12]], [[2006]]|accessdate=2006-06-12}}</ref> In all, about 350&nbsp;coastal residents took refuge in emergency shelters.<ref name="flncdc3"/> Prior to the arrival of the storm, Florida governor [[Jeb Bush]] declared a [[state of emergency]] for the state.<ref name="Jeb Bush EO">{{cite web|author=Bush, Jeb|year=2006|title=Executive Order Number 06-130- Tropical Storm Alberto|accessdate=2006-06-12|url=http://www.floridadisaster.org/eoc/eoc_activations/ExecOrders/2006-06-12%20EO%20TS%20Alberto.pdf}}</ref> A [[Tropical cyclone warnings and watches#Tropical Storm Watch|tropical storm watch]] was first issued for portions of the [[Florida Panhandle]] about 43&nbsp;hours prior to landfall. As Alberto was predicted to continue intensifying, the National Hurricane Center issued a [[Tropical cyclone warnings and watches#Hurricane Warning|hurricane warning]] from [[Longboat Key, Florida|Longboat Key]] to the mouth of the [[Ochlockonee River]] approximately 25&nbsp;hours before landfall. A tropical storm warning extended southward to [[Englewood, Florida|Englewood]] and westward to [[Indian Pass, Florida|Indian Pass]]. A tropical storm warning was also issued from [[Flagler Beach, Florida]] to the mouth of the [[Santee River]] in [[South Carolina]].<ref name="tcr"/> As the storm moved inland, local [[National Weather Service]] offices issued flood watches for portions of [[North Carolina]], [[Virginia]], and the [[Delmarva Peninsula]]. Additionally, flood and flash flood warnings were issued for some portions of the country from [[South Carolina]] through Virginia.<ref name="hpc19"/>
In northwestern Florida, officials issued a mandatory evacuation order a day before the storm moved ashore for about 21,000&nbsp;citizens in [[Levy County, Florida|Levy County]], [[Citrus County, Florida|Citrus County]], and [[Taylor County, Florida|Taylor County]].<ref>{{cite news|url=http://abclocal.go.com/wpvi/story?section=weather&id=4261181&pt=print|title=20,000 ordered to leave Florida's Gulf Coast|publisher=[[Associated Press]]|date=[[June 12]], [[2006]]|accessdate=2006-06-13}}</ref> Several schools were closed as well, and converted into shelters.<ref>{{cite news|url=http://www.tampabays10.com/news/local/article.aspx?storyid=33249|title=Hernando County issues a recommended evacuation of Zone A/B|publisher=[[WTSP]]|date=[[June 12]], [[2006]]|accessdate=2006-06-12}}</ref> In all, about 350&nbsp;coastal residents took refuge in emergency shelters.<ref name="flncdc3"/> Prior to the arrival of the storm, Florida governor [[Jeb Bush]] declared a [[state of emergency]] for the state.<ref name="Jeb Bush EO">{{cite web|author=Bush, Jeb|year=2006|title=Executive Order Number 06-130- Tropical Storm Alberto|accessdate=2006-06-12|url=http://www.floridadisaster.org/eoc/eoc_activations/ExecOrders/2006-06-12%20EO%20TS%20Alberto.pdf}}</ref> A [[Tropical cyclone warnings and watches#Tropical Storm Watch|tropical storm watch]] was first issued for portions of the [[Florida Panhandle]] about 43&nbsp;hours prior to landfall. As Alberto was predicted to continue intensifying, the National Hurricane Center issued a [[Tropical cyclone warnings and watches#Hurricane Warning|hurricane warning]] from [[Longboat Key, Florida|Longboat Key]] to the mouth of the [[Ochlockonee River]] approximately 25&nbsp;hours before landfall. A tropical storm warning extended southward to [[Englewood, Florida|Englewood]] and westward to [[Indian Pass, Florida|Indian Pass]]. A tropical storm warning was also issued from [[Flagler Beach, Florida]] to the mouth of the [[Santee River]] in [[South Carolina]].<ref name="tcr"/> As the storm moved inland, local [[National Weather Service]] offices issued flood watches for portions of [[North Carolina]], [[Virginia]], and the [[Delmarva Peninsula]]. Additionally, flood and flash flood warnings were issued for some portions of the country from [[South Carolina]] through Virginia.<ref name="hpc19"/>


While Alberto was becoming extratropical over land, the [[Canadian Hurricane Centre]] issued gale warnings for offshore waters of [[Nova Scotia]],<ref name="chc614">{{cite web|author=LaFortune|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060614055303.Alberto.txt.en}}</ref> and later for [[Newfoundland and Labrador|Newfoundland]]. In addition, the Atlantic Storm Prediction Center issued inland wind warnings for coastal regions of Nova Scotia.<ref name="chc615">{{cite web|author=LaFortune & Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 15, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615060241.Alberto.txt.en}}</ref> Due to the threat for precipitation, the Atlantic Storm Prediction Center posted rainfall warnings for all Atlantic coastal regions of Nova Scotia.<ref name="chc6142">{{cite web|author=LaFortune & Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006 (2)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060614232501.Alberto.txt.en}}</ref>
While Alberto was becoming extratropical over land, the [[Canadian Hurricane Centre]] issued gale warnings for offshore waters of [[Nova Scotia]],<ref name="chc614">{{cite web|author=LaFortune|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060614055303.Alberto.txt.en}}</ref> and later for [[Newfoundland and Labrador|Newfoundland]]. In addition, the Atlantic Storm Prediction Center issued inland wind warnings for coastal regions of Nova Scotia.<ref name="chc615">{{cite web|author=LaFortune & Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 15, 2006|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615060241.Alberto.txt.en}}</ref> Due to the prediction for precipitation, the Atlantic Storm Prediction Center posted rainfall warnings for all Atlantic coastal regions of Nova Scotia.<ref name="chc6142">{{cite web|author=LaFortune & Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006 (2)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060614232501.Alberto.txt.en}}</ref>


==Impact==
==Impact==
[[Image:alberto2006filledrainblk.GIF|thumb|right|Storm Rainfall in the United States]]
[[Image:alberto2006filledrainblk.GIF|thumb|right|Storm Rainfall in the United States]]
===Caribbean===
===Caribbean===
Early in its duration, the tropical depression which later became Alberto produced heavy rainfall across the western [[Caribbean Sea]]. A station on [[Grand Cayman]] reported 22.72&nbsp;inches (577&nbsp;mm) in one 24-hour period.<ref name="pa2">{{cite web|author=Knabb|year=2006|title=Tropical Depression One Public Advisory Two|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.public.002.shtml?}}</ref> In [[Cuba]], rainfall peaked at 17.52&nbsp;inches (445&nbsp;mm) in [[Pinar del Río]] province. On the [[Isle of Youth]], precipitation reached a maximum of 15.67&nbsp;inches (398&nbsp;mm) at [[Sumidero, Isle of Youth|Sumidero]], and in [[Havana Province]] rainfall reached 8.46&nbsp;inches (215&nbsp;mm) at [[Playa Baracoa Airport|Playa Baracoa]].<ref name="tcr"/> Much of the precipitation fell during a fairly short time, and was beneficial, as the area had been suffering from severe drought conditions.<ref name="cubwmo">{{cite web|author=Cuban delegates to the World Meteorological Organization|year=2007|title=Reports of hurricanes, tropical storms, tropical disturbances and related flooding during 2006 in Cuba|accessdate=2007-05-10|url=http://www.wmo.ch/pages/prog/www/tcp/documents/HC29_final_report-english.pdf|format=PDF}}</ref> In [[Havana, Cuba|Havana]], the rainfall damaged more than 40&nbsp;homes, 3 of which collapsed completely; this forced the evacuation of 284&nbsp;people.<ref name="cubeff"/>
In its early stages of development, the tropical depression which later became Alberto produced heavy rainfall across the western [[Caribbean Sea]]. A station on [[Grand Cayman]] reported 22.72&nbsp;inches (577&nbsp;mm) in one 24-hour period.<ref name="pa2">{{cite web|author=Knabb|year=2006|title=Tropical Depression One Public Advisory Two|publisher=National Hurricane Center|accessdate=2007-05-10|url=http://www.nhc.noaa.gov/archive/2006/al01/al012006.public.002.shtml?}}</ref> In [[Cuba]], rainfall amounted to 17.52&nbsp;inches (445&nbsp;mm) in [[Pinar del Río]] province,<ref name="tcr"/> where one station recorded 4.06&nbsp;inches (103&nbsp;mm) in one hour.<ref name="ips615"/> On the [[Isle of Youth]], precipitation accrued to 15.67&nbsp;inches (398&nbsp;mm) in [[Sumidero, Isle of Youth|Sumidero]].<ref name="tcr"/> Air and marine travel was disrupted between the Cuban mainland and the Isle of Youth.<ref name="afp612"/> In [[Havana Province]] rainfall totaled 8.46&nbsp;inches (215&nbsp;mm) at [[Playa Baracoa Airport|Playa Baracoa]].<ref name="tcr"/> Much of the precipitation fell during a fairly short time, and was beneficial, as the area had been suffering from severe drought conditions.<ref name="cubwmo">{{cite web|author=Cuban delegates to the World Meteorological Organization|year=2007|title=Reports of hurricanes, tropical storms, tropical disturbances and related flooding during 2006 in Cuba|accessdate=2007-05-10|url=http://www.wmo.ch/pages/prog/www/tcp/documents/HC29_final_report-english.pdf|format=PDF}}</ref> In Pinar del Río province, the precipitation flooded 50&nbsp;[[Square mile|sq mi]] (130&nbsp;[[Square kilometre|km<sup>2</sup>]] of crop land. The storm damaged about 50&nbsp;houses across the country, about half of which in [[Havana]].<ref name="ips615"/>


Alberto dropped light amounts of rainfall across [[Mexico]], with a 24-hour total peaking at 4&nbsp;inches (100&nbsp;mm) in [[Peto, Yucatán]]. Light rain was also reported throughout [[Quintana Roo]] and in eastern [[Campeche]].<ref name="smnalbe">{{cite web|author=Alberto Hernández Unzón|year=2006|title=Resumen de la Tormenta Tropical "Alberto" del Océano Atlántico|publisher=Servicio Meteorológico Nacional|accessdate=2007-05-11|url=http://smn.cna.gob.mx/ciclones/tempo2006/atlantico/alberto/alberto.pdf}}</ref>
Alberto dropped light amounts of rainfall across [[Mexico]], with a 24-hour total peaking at 4&nbsp;inches (100&nbsp;mm) in [[Peto, Yucatán]]. Light rain was also reported throughout [[Quintana Roo]] and in eastern [[Campeche]].<ref name="smnalbe">{{cite web|author=Alberto Hernández Unzón|year=2006|title=Resumen de la Tormenta Tropical "Alberto" del Océano Atlántico|publisher=Servicio Meteorológico Nacional|accessdate=2007-05-11|url=http://smn.cna.gob.mx/ciclones/tempo2006/atlantico/alberto/alberto.pdf}}</ref>


===Florida===
===Florida===
The large area of convection associated with Alberto dropped rainfall across Florida for several days. The statewide precipitation maximum reached 7.08&nbsp;inches (180&nbsp;mm) at a station 5&nbsp;miles (8&nbsp;km) east of [[Tarpon Springs, Florida|Tarpon Springs]].<ref name="flncdc">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607421}}</ref> The highest sustained winds from the storm were officially clocked at 40&nbsp;mph (65&nbsp;km/h) in [[Saint Petersburg, Florida|St. Petersburg]], which also saw reports of [[wind gusts]] of up to 56&nbsp;mph (90&nbsp;km/h). Upon making landfall on the [[Florida Panhandle]], the storm produced a [[storm tide]] which reached an unofficial peak of 7.3&nbsp;feet (2.2&nbsp;m) at [[Crystal River 3 Nuclear Generating Station|Crystal River Power Plant]].<ref name="tcr"/> The combination of high surf and the storm tide caused surge flooding along the [[Florida Panhandle]].<ref name="talnws">{{cite web|author=Tallahassee, Florida National Weather Service|year=2006|title=Tropical Storm Alberto 2006|publisher=NOAA|accessdate=2007-05-21|url=http://www.srh.noaa.gov/tlh/tropical/alberto06.html}}</ref> Six tornadoes were spawned in the state from the outer rainbands of Alberto, none of which caused serious damage.<ref name="flncdc2">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (2)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607423}}</ref><ref name="flncdc3">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (3)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607443}}</ref>
The large area of convection associated with Alberto dropped rainfall across Florida for several days. The statewide precipitation maximum reached 7.08&nbsp;inches (180&nbsp;mm) at a station 5&nbsp;miles (8&nbsp;km) east of [[Tarpon Springs, Florida|Tarpon Springs]].<ref name="flncdc">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607421}}</ref> The highest sustained winds from the storm were officially clocked at 40&nbsp;mph (65&nbsp;km/h) in [[Saint Petersburg, Florida|St. Petersburg]], which also saw reports of [[Gust (wind)|wind gusts]] of up to 56&nbsp;mph (90&nbsp;km/h). Upon making landfall on the [[Florida Panhandle]], the storm produced a [[storm tide]] which unofficially peaked at 7.3&nbsp;feet (2.2&nbsp;m) at [[Crystal River 3 Nuclear Generating Station|Crystal River Power Plant]].<ref name="tcr"/> The combination of high surf and the storm tide caused surge flooding along the [[Florida Panhandle]].<ref name="talnws">{{cite web|author=Tallahassee, Florida National Weather Service|year=2006|title=Tropical Storm Alberto 2006|publisher=NOAA|accessdate=2007-05-21|url=http://www.srh.noaa.gov/tlh/tropical/alberto06.html}}</ref> Six tornadoes were spawned in the state from the outer rainbands of Alberto, none of which caused serious damage.<ref name="flncdc2">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (2)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607423}}</ref><ref name="flncdc3">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (3)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607443}}</ref>
[[Image:alberto-flooding.jpg|thumb|right|Storm surge flooding from Tropical Storm Alberto at [[Horseshoe Beach, Florida]]]]
[[Image:alberto-flooding.jpg|thumb|right|Storm surge flooding from Tropical Storm Alberto at [[Horseshoe Beach, Florida]]]]
Across coastal areas, the storm surge flooding caused minor damage to dozens of homes and closed several roads. Near [[Homosassa, Florida|Homosassa]], two people who did not evacuate required water rescue. At [[Egmont Key State Park]], a woman fell overboard when a band of showers and surging currents made navigation difficult; her husband and a friend drowned after jumping in to save her without life jackets, though the woman returned safely to the boat.<ref name="flncdc3"/> The rainfall caused some temporary road flooding, though it was mostly beneficial in alleviating drought conditions. Moderate wind gusts caused scattered power outages and downed some trees across the northeast portion of the state.<ref name="flncdc2"/> Overall, property damage in the state rose to about $390,000 (2006&nbsp;USD) in total.<ref name="flncdc3"/><ref name="flncdc4">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (4)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607440}}</ref>
Across coastal areas, the storm surge flooding caused minor damage to dozens of homes and closed several roads. Near [[Homosassa, Florida|Homosassa]], two people who did not evacuate required water rescue. At [[Egmont Key State Park]], a woman fell off of a boat when a band of showers and surging currents made navigation difficult; her husband and a friend drowned after jumping in to save her without life jackets, though the woman returned safely to the boat.<ref name="flncdc3"/> The rainfall caused some temporary road flooding, though precipitation was mostly beneficial in alleviating drought conditions. Moderate wind gusts caused scattered power outages and downed some trees across the northeast portion of the state.<ref name="flncdc2"/> Overall, property damage in the state rose to about $390,000 (2006&nbsp;USD) in total.<ref name="flncdc3"/><ref name="flncdc4">{{cite web|author=National Climatic Data Center|accessdate=2007-05-21|year=2006|title=Event Report for Florida (4)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~607440}}</ref>


Shortly before Alberto moved ashore, the [[United States Coast Guard]] began searching off of [[Boynton Beach, Florida|Boynton Beach]] for a missing boat after police received a call of a lost boat with nine people. After searching for about 24&nbsp;hours<ref name="ap613">{{cite web|author=Associated Press|year=2006|title=Coast Guard ends search for ‘missing’ boaters|accessdate=2007-05-21|url=http://www.msnbc.msn.com/id/13119208/}}</ref> at a cost of $278,000,<ref name="sfs614">{{cite web|author=Leon Fooksman|year=2006|title= Possible sinking-boat hoax cost $278,000 for daylong air and sea search|publisher=South Florida Sun-Sentinel|accessdate=2007-05-21|url=http://www.highbeam.com/doc/1G1-146999516.html}}</ref> officials determined it to be a hoax, and imprisoned the man responsible for 30&nbsp;months.<ref>{{cite web|author=The United States Attorney's Office|year=2006|title=Boynton Beach Man Sentenced to Prison for Making Hoax Distress Call to the Coast Guard|accessdate=2007-05-21|url=http://www.usdoj.gov/usao/fls/PressReleases/061031-01.html}}</ref>
Shortly before Alberto moved ashore, the [[United States Coast Guard]] began searching off of [[Boynton Beach, Florida|Boynton Beach]] for a missing boat after police received a call of a lost boat with nine people. After searching for about 24&nbsp;hours<ref name="ap613">{{cite web|author=Associated Press|year=2006|title=Coast Guard ends search for ‘missing’ boaters|accessdate=2007-05-21|url=http://www.msnbc.msn.com/id/13119208/}}</ref> at a cost of $278,000,<ref name="sfs614">{{cite web|author=Leon Fooksman|year=2006|title= Possible sinking-boat hoax cost $278,000 for daylong air and sea search|publisher=South Florida Sun-Sentinel|accessdate=2007-05-21|url=http://www.highbeam.com/doc/1G1-146999516.html}}</ref> officials determined it to be a hoax. The man responsible for the incident was sentenced to prison for 30&nbsp;months, after being charged with making a hoax distress call to the Coast Guard.<ref>{{cite web|author=The United States Attorney's Office|year=2006|title=Boynton Beach Man Sentenced to Prison for Making Hoax Distress Call to the Coast Guard|accessdate=2007-05-21|url=http://www.usdoj.gov/usao/fls/PressReleases/061031-01.html}}</ref>


===Southeast United States===
===Southeast United States===
[[Image:Alberto NC flooding - edit.jpg|right|thumb|Flooding in North Carolina from Alberto]]
[[Image:Alberto NC flooding - edit.jpg|right|thumb|Flooding in North Carolina from Alberto]]
While the storm moved through the state of [[Georgia (U.S. state)|Georgia]], moderate winds occurred along the coastline, with wind gusts officially peaking at 45&nbsp;mph (72&nbsp;km/h).<ref name="tcr"/> Rainfall ranged from 3&ndash;5&nbsp;inches (75&ndash;125&nbsp;mm) across the southeast portion of the state,<ref name="gancdc">{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for Georgia|accessdate=2007-05-18 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~608426}}</ref> with isolated higher totals peaking at 7.05&nbsp;inches (179&nbsp;mm) in [[Rincon, Georgia|Rincon]].<ref name="hpc19"/> Alberto produced a [[storm tide]] of 8.53&nbsp;feet (2.6&nbsp;m) at [[Fort Pulaski National Monument]], causing some [[beach erosion]] reported along the coastline.<ref name="scnws"/>
While the storm moved through the state of [[Georgia (U.S. state)|Georgia]], moderate winds of up to 45&nbsp;mph (72&nbsp;km/h) occurred along the coastline.<ref name="tcr"/> Rainfall ranged from 3&ndash;5&nbsp;inches (75&ndash;125&nbsp;mm) across the southeast portion of the state,<ref name="gancdc">{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for Georgia|accessdate=2007-05-18 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~608426}}</ref> with isolated higher maxima of up to 7.05&nbsp;inches (179&nbsp;mm) in [[Rincon, Georgia|Rincon]].<ref name="hpc19"/> Alberto produced a [[storm tide]] of 8.53&nbsp;feet (2.6&nbsp;m) at [[Fort Pulaski National Monument]], causing some [[beach erosion]] reported along the coastline.<ref name="scnws"/>


Alberto produced tropical storm force winds along the [[South Carolina]] coastline; the highest official wind gust was 51&nbsp;mph (82&nbsp;km/h) at [[Edisto Beach, South Carolina|Edisto Beach]].<ref name="tcr"/> The storm dropped precipitation across much of the state, including a state maximum of 4.42&nbsp;inches (112&nbsp;mm) at [[Pritchardville, South Carolina|Pritchardville]]. [[Storm tide]]s reached 7.81&nbsp;feet (2.4&nbsp;m) above the mean low-level water mark along [[Fripp Island (South Carolina)|Fripp Island]], leading to some beach [[erosion]] along portions of the coastline. While in the process of becoming extratropical, the rainbands of Alberto spawned seven confirmed [[tornado]]es in the state, all of which but one rated [[Fujita scale|F0]];<ref name="tcr"/> a [[National Weather Service]] report indicated additional tornadoes may have occurred in the state. The tornadoes caused some minor damage, though overall damage in the state was minimal.<ref name="scnws">{{cite web|author=Charleston, South Carolina National Weather Service |year=2006 |title=Tropical Storm Alberto Post Tropical Cyclone Report |publisher=NOAA |accessdate=2007-05-18 |url=http://www.erh.noaa.gov/chs/text/PSHCHS_06152006_2117.txt}}</ref>
Alberto produced winds of tropical storm force along the [[South Carolina]] coastline; the highest official wind gust was 51&nbsp;mph (82&nbsp;km/h) at [[Edisto Beach, South Carolina|Edisto Beach]].<ref name="tcr"/> The storm dropped precipitation across much of the state, including a state maximum of 4.42&nbsp;inches (112&nbsp;mm) at [[Pritchardville, South Carolina|Pritchardville]]. [[Storm tide]]s reached 7.81&nbsp;feet (2.4&nbsp;m) above the mean low-level water mark along [[Fripp Island (South Carolina)|Fripp Island]], leading to some beach [[erosion]] along portions of the coastline. While in the process of becoming extratropical, the rainbands of Alberto spawned seven confirmed [[tornado]]es in the state, most of which rated [[Fujita scale|F0]];<ref name="tcr"/> a [[National Weather Service]] report indicated additional tornadoes may have occurred in the state. The tornadoes caused some minor damage, though overall damage in the state was minimal.<ref name="scnws">{{cite web|author=Charleston, South Carolina National Weather Service |year=2006 |title=Tropical Storm Alberto Post Tropical Cyclone Report |publisher=NOAA |accessdate=2007-05-18 |url=http://www.erh.noaa.gov/chs/text/PSHCHS_06152006_2117.txt}}</ref>


The remnants of Alberto dropped heavy precipitation across [[North Carolina]], including a nation-wide high of 7.16&nbsp;inches (182&nbsp;mm) at the [[Raleigh, North Carolina|Raleigh]] National Weather Service Office.<ref name="rain"/> Some totals broke previous rainfall records,<ref name="ncrainbroke">{{cite web|author=Blaes|year=2006|title=Remnants of Alberto Produced Record Rainfall Amounts Across Central North Carolina|publisher=Raleigh, North Carolina National Weather Service |accessdate=2007-05-20 |url=http://www4.ncsu.edu/~nwsfo/storage/cases/20060614/20060615.RDUPNSRAH.html}}</ref> including the station at [[Raleigh-Durham International Airport]] which broke the all-time daily precipitation record for that station. The rainfall led to flooding across the central portion of the state, with 45&nbsp;flash flood warnings issued by the Raleigh National Weather Service. Police and firefighters in [[Wake County, North Carolina|Wake County]] performed 47&nbsp;water rescues. Additionally, the Raleigh-Wake [[9-1-1]]&nbsp;center received more than 1,076&nbsp;calls for help. Flash flooding occurred throughout the area, which caused the [[Crabtree Creek]] in Raleigh to crest at 23.77&nbsp;feet (7.2&nbsp;m);<ref name="ralnws">{{cite web|author=Raleigh, NC National Weather Service|year=2006|title=Tropical Storm Alberto Event Summary|accessdate=2007-05-20|url=http://www4.ncsu.edu/~nwsfo/storage/cases/20060614/}}</ref> this was the second highest flood stage on record for the creek. The overflown creek flooded a few cars to their rooftops, and resulted in the closure of the [[Crabtree Valley Mall]]. Major flooding was reported elsewhere throughout the region, which closed several roads and damaged some houses.<ref name="abc11">{{cite web|author=ABC11TV|year=2006|title=Alberto Brings Worst Flooding Since Fran|accessdate=2007-05-20|url=http://abclocal.go.com/wtvd/story?section=central&id=4265148}}</ref> In [[Franklin County, North Carolina|Franklin County]], an eight year-old boy drowned after getting sucked into a flooded drainage system; the death is considered indirect because the boy was chasing a ball into the drainage system.<ref name="tcr"/> Near the coast, the storm produced several [[waterspout]]s, some of which moved ashore in [[Dare County, North Carolina|Dare]] and [[Carteret County, North Carolina|Carteret counties]];<ref name="ncncdc">{{cite web|author=National Climatic Data Center|accessdate=2007-05-20|year=2006|title=Event Report for North Carolina|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~627897}}</ref> an F0 tornado struck [[Morehead City, North Carolina|Morehead City]].<ref name="ncncdc3">{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for North Carolina (2) |accessdate=2007-05-20 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~627888}}</ref> Wind gusts reached 60&nbsp;mph (95&nbsp;km/h), resulting in downed trees and a damaged barn.<ref name="ncncdc2">{{cite web|author=National Climatic Data Center|accessdate=2007-05-20|year=2006|title=Event Report for North Carolina (3)|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~627898}}</ref> Damage across the state totaled about $30,000 (2006&nbsp;USD).<ref name="ncncdc2"/><ref name="ncncdc3"/>
The remnants of Alberto dropped heavy precipitation across [[North Carolina]], including a nation-wide high of 7.16&nbsp;inches (182&nbsp;mm) at the [[Raleigh, North Carolina|Raleigh]] National Weather Service Office.<ref name="rain"/> Some totals broke previous rainfall records,<ref name="ncrainbroke">{{cite web|author=Blaes|year=2006|title=Remnants of Alberto Produced Record Rainfall Amounts Across Central North Carolina|publisher=Raleigh, North Carolina National Weather Service |accessdate=2007-05-20 |url=http://www4.ncsu.edu/~nwsfo/storage/cases/20060614/20060615.RDUPNSRAH.html}}</ref> including the station at [[Raleigh-Durham International Airport]] which broke the all-time daily precipitation record for that station. The rainfall led to flooding across the central portion of the state, with 45&nbsp;flash flood warnings issued by the Raleigh National Weather Service. Police and firefighters in [[Wake County, North Carolina|Wake County]] performed 47&nbsp;water rescues. Additionally, the Raleigh-Wake [[9-1-1]]&nbsp;center received more than 1,076&nbsp;calls for help. Flash flooding occurred throughout the area, which caused the [[Crabtree Creek]] in Raleigh to crest at 23.77&nbsp;feet (7.2&nbsp;m);<ref name="ralnws">{{cite web|author=Raleigh, NC National Weather Service|year=2006|title=Tropical Storm Alberto Event Summary|accessdate=2007-05-20|url=http://www4.ncsu.edu/~nwsfo/storage/cases/20060614/}}</ref> this was the second highest flood stage on record for the creek. The overflown creek flooded a few cars to their rooftops, and resulted in the closure of the [[Crabtree Valley Mall]]. Major flooding was reported elsewhere throughout the region, which closed several roads and damaged some houses.<ref name="abc11">{{cite web|author=ABC11TV|year=2006|title=Alberto Brings Worst Flooding Since Fran|accessdate=2007-05-20|url=http://abclocal.go.com/wtvd/story?section=central&id=4265148}}</ref> In [[Franklin County, North Carolina|Franklin County]], an eight year-old boy drowned after getting sucked into a flooded drainage system; the death is considered indirect because the boy was chasing a ball into the drainage system.<ref name="tcr"/> Near the coast, the storm produced several [[waterspout]]s, some of which moved ashore in [[Dare County, North Carolina|Dare]] and [[Carteret County, North Carolina|Carteret counties]]. Isolated reports of 60&nbsp;mph (95&nbsp;km/h) wind gusts resulted in downed trees and minor damage.<ref>{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for North Carolina|accessdate=2008-02-12|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~627880}}</ref>


Rainfall from the storm extended into [[Virginia]], the [[Eastern Shore of Maryland]], and extreme southeastern [[Delaware]].<ref name="rain"/> Precipitation reached 5.8&nbsp;inches (147&nbsp;mm) in [[Virginia Beach]],<ref name="waknws">{{cite web|author=Cullen|year=2006|title=Tropical Storm Alberto Post-Storm Report|publisher=Wakefield, Virginia National Weather Service|accessdate=2007-05-20 |url=http://www.erh.noaa.gov/er/akq/wx_events/hur/alberto_2006.txt}}</ref> which caused flash flooding in the [[Hampton Roads]] area. The flooding closed several roads, though no major damage was reported.<ref name="vancdc">{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for Virginia |accessdate=2007-05-20 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~638874}}</ref>
Rainfall from the storm extended into [[Virginia]], the [[Eastern Shore of Maryland]], and extreme southeastern [[Delaware]].<ref name="rain"/> Precipitation totaled 5.8&nbsp;inches (147&nbsp;mm) in [[Virginia Beach]],<ref name="waknws">{{cite web|author=Cullen|year=2006|title=Tropical Storm Alberto Post-Storm Report|publisher=Wakefield, Virginia National Weather Service|accessdate=2007-05-20 |url=http://www.erh.noaa.gov/er/akq/wx_events/hur/alberto_2006.txt}}</ref> which caused flash flooding in the [[Hampton Roads]] area. The flooding closed several roads, though no major damage was reported.<ref name="vancdc">{{cite web|author=National Climatic Data Center|year=2006|title=Event Report for Virginia |accessdate=2007-05-20 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~638874}}</ref>


===Canada===
===Canada===
The extratropical remnant of Alberto produced strong winds across the [[Canada|Canadian]] [[Maritimes]], with gusts peaking at 74&nbsp;mph (119&nbsp;km/h) in the [[Barrington, Nova Scotia|Barrington]] district of [[Nova Scotia]].<ref name="chc6152"/> Sustained winds reached 51&nbsp;mph (83&nbsp;km/h), as well.<ref name="chc"/> Rainfall from the storm was moderate, with some locations reporting 0.4&nbsp;inches (10&nbsp;mm) per hour;<ref name="chc6153">{{cite web|author=Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006 (3)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615180233.Alberto.txt.en}}</ref> totals exceeded 2&nbsp;inches (50&nbsp;mm) in numerous areas. Due to wet grounds, the winds knocked down some trees and several tree limbs, and also downed some power lines,<ref name="chc6152"/> causing localized power outages.<ref name="chc"/> Moderate winds and rainfall affected [[Newfoundland and Labrador|Newfoundland]], as well.<ref name="chc616"/> According to a press report, the passage of the storm left four sailors missing about 230&nbsp;miles (370&nbsp;km) south of Nova Scotia.<ref name="tcr"/>
The extratropical remnant of Alberto produced strong winds across the [[Canada|Canadian]] [[Maritimes]], including gusts of 74&nbsp;mph (119&nbsp;km/h) in the [[Barrington, Nova Scotia|Barrington]] district of [[Nova Scotia]].<ref name="chc6152"/> Sustained winds reached 51&nbsp;mph (83&nbsp;km/h).<ref name="chc"/> Rainfall from the storm was moderate, with some locations reporting 0.4&nbsp;inches (10&nbsp;mm) per hour;<ref name="chc6153">{{cite web|author=Bowyer|year=2006|title=Tropical Storm Alberto Information Statement for June 14, 2006 (3)|publisher=Canadian Hurricane Centre|accessdate=2007-05-10|url=http://www.atl.ec.gc.ca/weather/hurricane/bulletins/20060615180233.Alberto.txt.en}}</ref> totals exceeded 2&nbsp;inches (50&nbsp;mm) in numerous areas. Due to wet grounds, the winds knocked down some trees and several tree limbs, and also downed some power lines,<ref name="chc6152"/> causing localized power outages.<ref name="chc"/> Moderate winds and rainfall affected [[Newfoundland and Labrador|Newfoundland]], as well.<ref name="chc616"/> According to a press report, the passage of the storm left four sailors missing about 230&nbsp;miles (370&nbsp;km) south of Nova Scotia.<ref name="tcr"/>


==See also==
==See also==

Revision as of 02:56, 13 February 2008

Tropical Storm Alberto
Tropical storm (SSHWS/NWS)
Tropical Storm Alberto near peak strength
FormedJune 10, 2006
DissipatedJune 14, 2006
Highest winds1-minute sustained: 70 mph (110 km/h)
Lowest pressure995 mbar (hPa); 29.38 inHg
Fatalities3 indirect, 4 missing
Damage$420,000 (2006 USD)
Areas affectedNorthwest Caribbean Sea, Southeast United States Landfall in Florida, Atlantic Canada
Part of the 2006 Atlantic hurricane season

Tropical Storm Alberto was the first tropical storm of the 2006 Atlantic hurricane season. Forming on June 10 in the northwestern Caribbean Sea, the storm moved generally to the north, reaching a maximum intensity of 70 mph (110 km/h) before weakening and moving ashore in the Big Bend area of Florida on June 13. Alberto then moved through eastern Georgia, North Carolina, and Virginia as a tropical depression before becoming extratropical on June 14.

Across the western Caribbean, the storm produced heavy rainfall, causing some minor damage. In Florida, a moderate storm tide caused coastal damage and flooding, while Alberto's outer rainbands produced several tornadoes. The storm was indirectly responsible for two drownings off the coast of Tampa Bay. In North Carolina, heavy rainfall caused locally severe flooding, and one person drowned after running into a flooded storm drain near Raleigh. The remnants of Alberto produced strong winds and left four people missing in Atlantic Canada. Overall, damage was minor along Alberto's path.

Storm history

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
Saffir–Simpson scale
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

In early June 2006, an area of convection persisted across Central America and the western Caribbean Sea, in association with a broad, nearly stationary trough of low pressure.[1][2] Thunderstorms increased and became more concentrated on June 8 after a tropical wave moved into the western Caribbean,[1] and an upper-level low to its west increased outflow over the system.[3] The disturbance moved slowly north-northwestward, and development was initially inhibited by marginally favorable upper-level winds and land interaction.[4] The system gradually organized,[5] and by June 10 a circulation formed with sufficiently organized convection for the National Hurricane Center to classify it Tropical Depression One. At this point the storm was located about 140 miles (225 km) south of the western tip of Cuba.[1]

The depression tracked to the northwest through the Yucatán Channel into an area of increased wind shear, which the center exposed and elongated.[1][6] Despite its poor structure, the system maintained strong winds in its eastern semicircle. The depression intensified into Tropical Storm Alberto early on June 11 about 260 miles (420 km) southwest of the Dry Tortugas, based on Hurricane Hunters' reports of flight level winds of 50 mph (80 km/h) in a few convective bands.[1] Upon becoming a tropical storm, the low-level circulation had become better defined, though forecasts predicted the wind shear would increase, preventing significant strengthening of the storm.[7] One forecaster at the National Hurricane Center remarked the system resembled a subtropical cyclone.[8] However, deep convection developed and built westward against the wind shear as the overall organization improved. At the same time Alberto turned northeastward under the influence of an approaching trough.[9] On June 12, the circulation abruptly reformed under the area of deepest convection, which coincided with the storm's passage over the loop current; consequentially, Alberto quickly strengthened to reach peak winds of 70 mph (115 km/h) about 220 miles (350 km) west-northwest of Tampa, Florida.[1]

Though it was projected to track over cooler waters and stay in an area of increased shear, forecasters at the National Hurricane Center predicted Alberto to attain hurricane status and make landfall at that intensity.[10] The storm maintained peak intensity for about 18 hours,[1] and while accelerating northeastward, Alberto's convection diminished as the cloud pattern became elongated.[11] On June 13, dry air became entrained in the circulation, leaving the center exposed from the convection and the wind field greatly broadened.[12] A partial eyewall developed in the western semicircle of the center; however, winds were well below hurricane force.[13] Alberto continued to weaken, and made landfall at about 1630 UTC on June 13 with 45 mph (75 km/h) winds in Taylor County, Florida, about 50 miles (80 km) southeast of Tallahassee.[1]

Tropical Storm Alberto over South Carolina

The storm maintained a well-organized structure[14] and banding features over land,[15] and Alberto continued to produce winds of tropical storm force as it moved into Georgia. Early on June 14, the storm weakened to tropical depression status while located near the city of Millen, Georgia. Alberto began to lose tropical characteristics soon thereafter, and about six hours after weakening to a tropical depression it transitioned into an extratropical cyclone.[1] Late on June 14 it accelerated northeastward to emerge into the Atlantic Ocean,[16] and on June 15, it entered the area of responsibility of the Canadian Hurricane Centre.[17] While over open waters, Alberto's remnants began to re-intensify; later that day, the extratropical remnant low attained winds of 65 mph (105 km/h) and a pressure of 969 mbar while a short distance south of Nova Scotia.[1] At this time, the low presented a well-defined comma structure.[18] After passing near Sable Island,[18] the remnants of Alberto crossed the Avalon Peninsula of Newfoundland on June 16.[19] The extratropical storm turned to the east-northeast and later to the east as it continued its rapid forward motion, and on June 19 the remnants of Alberto merged with an approaching cold front near the British Isles.[1]

Preparations

Radar image of Tropical Storm Alberto at landfall

By June 12, the Cuban government had evacuated over 25,000 people in the western portion of the country due to the threat of flooding.[20][21] The National Hurricane Center recommended tropical storm warnings for the Isle of Youth and the Pinar del Rio province early on June 10, but they were not issued by the Cuban government.[22]

In northwestern Florida, officials issued a mandatory evacuation order a day before the storm moved ashore for about 21,000 citizens in Levy County, Citrus County, and Taylor County.[23] Several schools were closed as well, and converted into shelters.[24] In all, about 350 coastal residents took refuge in emergency shelters.[25] Prior to the arrival of the storm, Florida governor Jeb Bush declared a state of emergency for the state.[26] A tropical storm watch was first issued for portions of the Florida Panhandle about 43 hours prior to landfall. As Alberto was predicted to continue intensifying, the National Hurricane Center issued a hurricane warning from Longboat Key to the mouth of the Ochlockonee River approximately 25 hours before landfall. A tropical storm warning extended southward to Englewood and westward to Indian Pass. A tropical storm warning was also issued from Flagler Beach, Florida to the mouth of the Santee River in South Carolina.[1] As the storm moved inland, local National Weather Service offices issued flood watches for portions of North Carolina, Virginia, and the Delmarva Peninsula. Additionally, flood and flash flood warnings were issued for some portions of the country from South Carolina through Virginia.[16]

While Alberto was becoming extratropical over land, the Canadian Hurricane Centre issued gale warnings for offshore waters of Nova Scotia,[27] and later for Newfoundland. In addition, the Atlantic Storm Prediction Center issued inland wind warnings for coastal regions of Nova Scotia.[28] Due to the prediction for precipitation, the Atlantic Storm Prediction Center posted rainfall warnings for all Atlantic coastal regions of Nova Scotia.[29]

Impact

File:Alberto2006filledrainblk.GIF
Storm Rainfall in the United States

Caribbean

In its early stages of development, the tropical depression which later became Alberto produced heavy rainfall across the western Caribbean Sea. A station on Grand Cayman reported 22.72 inches (577 mm) in one 24-hour period.[22] In Cuba, rainfall amounted to 17.52 inches (445 mm) in Pinar del Río province,[1] where one station recorded 4.06 inches (103 mm) in one hour.[20] On the Isle of Youth, precipitation accrued to 15.67 inches (398 mm) in Sumidero.[1] Air and marine travel was disrupted between the Cuban mainland and the Isle of Youth.[21] In Havana Province rainfall totaled 8.46 inches (215 mm) at Playa Baracoa.[1] Much of the precipitation fell during a fairly short time, and was beneficial, as the area had been suffering from severe drought conditions.[30] In Pinar del Río province, the precipitation flooded 50 sq mi (130 km2 of crop land. The storm damaged about 50 houses across the country, about half of which in Havana.[20]

Alberto dropped light amounts of rainfall across Mexico, with a 24-hour total peaking at 4 inches (100 mm) in Peto, Yucatán. Light rain was also reported throughout Quintana Roo and in eastern Campeche.[31]

Florida

The large area of convection associated with Alberto dropped rainfall across Florida for several days. The statewide precipitation maximum reached 7.08 inches (180 mm) at a station 5 miles (8 km) east of Tarpon Springs.[32] The highest sustained winds from the storm were officially clocked at 40 mph (65 km/h) in St. Petersburg, which also saw reports of wind gusts of up to 56 mph (90 km/h). Upon making landfall on the Florida Panhandle, the storm produced a storm tide which unofficially peaked at 7.3 feet (2.2 m) at Crystal River Power Plant.[1] The combination of high surf and the storm tide caused surge flooding along the Florida Panhandle.[33] Six tornadoes were spawned in the state from the outer rainbands of Alberto, none of which caused serious damage.[34][25]

Storm surge flooding from Tropical Storm Alberto at Horseshoe Beach, Florida

Across coastal areas, the storm surge flooding caused minor damage to dozens of homes and closed several roads. Near Homosassa, two people who did not evacuate required water rescue. At Egmont Key State Park, a woman fell off of a boat when a band of showers and surging currents made navigation difficult; her husband and a friend drowned after jumping in to save her without life jackets, though the woman returned safely to the boat.[25] The rainfall caused some temporary road flooding, though precipitation was mostly beneficial in alleviating drought conditions. Moderate wind gusts caused scattered power outages and downed some trees across the northeast portion of the state.[34] Overall, property damage in the state rose to about $390,000 (2006 USD) in total.[25][35]

Shortly before Alberto moved ashore, the United States Coast Guard began searching off of Boynton Beach for a missing boat after police received a call of a lost boat with nine people. After searching for about 24 hours[36] at a cost of $278,000,[37] officials determined it to be a hoax. The man responsible for the incident was sentenced to prison for 30 months, after being charged with making a hoax distress call to the Coast Guard.[38]

Southeast United States

Flooding in North Carolina from Alberto

While the storm moved through the state of Georgia, moderate winds of up to 45 mph (72 km/h) occurred along the coastline.[1] Rainfall ranged from 3–5 inches (75–125 mm) across the southeast portion of the state,[39] with isolated higher maxima of up to 7.05 inches (179 mm) in Rincon.[16] Alberto produced a storm tide of 8.53 feet (2.6 m) at Fort Pulaski National Monument, causing some beach erosion reported along the coastline.[40]

Alberto produced winds of tropical storm force along the South Carolina coastline; the highest official wind gust was 51 mph (82 km/h) at Edisto Beach.[1] The storm dropped precipitation across much of the state, including a state maximum of 4.42 inches (112 mm) at Pritchardville. Storm tides reached 7.81 feet (2.4 m) above the mean low-level water mark along Fripp Island, leading to some beach erosion along portions of the coastline. While in the process of becoming extratropical, the rainbands of Alberto spawned seven confirmed tornadoes in the state, most of which rated F0;[1] a National Weather Service report indicated additional tornadoes may have occurred in the state. The tornadoes caused some minor damage, though overall damage in the state was minimal.[40]

The remnants of Alberto dropped heavy precipitation across North Carolina, including a nation-wide high of 7.16 inches (182 mm) at the Raleigh National Weather Service Office.[3] Some totals broke previous rainfall records,[41] including the station at Raleigh-Durham International Airport which broke the all-time daily precipitation record for that station. The rainfall led to flooding across the central portion of the state, with 45 flash flood warnings issued by the Raleigh National Weather Service. Police and firefighters in Wake County performed 47 water rescues. Additionally, the Raleigh-Wake 9-1-1 center received more than 1,076 calls for help. Flash flooding occurred throughout the area, which caused the Crabtree Creek in Raleigh to crest at 23.77 feet (7.2 m);[42] this was the second highest flood stage on record for the creek. The overflown creek flooded a few cars to their rooftops, and resulted in the closure of the Crabtree Valley Mall. Major flooding was reported elsewhere throughout the region, which closed several roads and damaged some houses.[43] In Franklin County, an eight year-old boy drowned after getting sucked into a flooded drainage system; the death is considered indirect because the boy was chasing a ball into the drainage system.[1] Near the coast, the storm produced several waterspouts, some of which moved ashore in Dare and Carteret counties. Isolated reports of 60 mph (95 km/h) wind gusts resulted in downed trees and minor damage.[44]

Rainfall from the storm extended into Virginia, the Eastern Shore of Maryland, and extreme southeastern Delaware.[3] Precipitation totaled 5.8 inches (147 mm) in Virginia Beach,[45] which caused flash flooding in the Hampton Roads area. The flooding closed several roads, though no major damage was reported.[46]

Canada

The extratropical remnant of Alberto produced strong winds across the Canadian Maritimes, including gusts of 74 mph (119 km/h) in the Barrington district of Nova Scotia.[18] Sustained winds reached 51 mph (83 km/h).[17] Rainfall from the storm was moderate, with some locations reporting 0.4 inches (10 mm) per hour;[47] totals exceeded 2 inches (50 mm) in numerous areas. Due to wet grounds, the winds knocked down some trees and several tree limbs, and also downed some power lines,[18] causing localized power outages.[17] Moderate winds and rainfall affected Newfoundland, as well.[19] According to a press report, the passage of the storm left four sailors missing about 230 miles (370 km) south of Nova Scotia.[1]

See also

Template:Tcportal

References

  1. ^ a b c d e f g h i j k l m n o p q r s t u Lixion Avila & Daniel Brown (2006). "Tropical Storm Alberto Tropical Cyclone Report" (PDF). National Hurricane Center. Retrieved 2007-05-10.
  2. ^ Pasch (2006). "June 6 Tropical Weather Outlook". National Hurricane Center. Retrieved 2007-05-10.
  3. ^ a b c David Roth (2006). "Tropical Storm Alberto - June 2006". Hydrometeorological Prediction Center. Retrieved 2007-05-10.
  4. ^ Stewart (2006). "June 8 Tropical Weather Outlook". National Hurricane Center. Retrieved 2007-05-10.
  5. ^ Mainelli/Knabb (2006). "June 9 Tropical Weather Outlook". National Hurricane Center. Retrieved 2007-05-10.
  6. ^ Beven (2006). "Tropical Depression One Special Discussion One". National Hurricane Center. Retrieved 2007-05-10.
  7. ^ Pasch (2006). "Tropical Storm Alberto Discussion Six". National Hurricane Center. Retrieved 2007-05-10.
  8. ^ Pasch (2006). "Tropical Storm Alberto Discussion Seven". National Hurricane Center. Retrieved 2007-05-10.
  9. ^ Franklin (2006). "Tropical Storm Alberto Discussion Nine". National Hurricane Center. Retrieved 2007-05-10.
  10. ^ Pasch (2006). "Tropical Storm Alberto Discussion Ten". National Hurricane Center. Retrieved 2007-05-10.
  11. ^ Pasch (2006). "Tropical Storm Alberto Discussion Eleven". National Hurricane Center. Retrieved 2007-05-10.
  12. ^ Franklin (2006). "Tropical Storm Alberto Discussion Thirteen". National Hurricane Center. Retrieved 2007-05-10.
  13. ^ Pasch (2006). "Tropical Storm Alberto Discussion Fourteen". National Hurricane Center. Retrieved 2007-05-10.
  14. ^ Pasch (2006). "Tropical Storm Alberto Discussion Fifteen". National Hurricane Center. Retrieved 2007-05-10.
  15. ^ Stewart (2006). "Tropical Storm Alberto Discussion Sixteen". National Hurricane Center. Retrieved 2007-05-10.
  16. ^ a b c Fries & Petersen (2006). "Public Advisory 19 on Remnants of Alberto". Hydrometeorological Prediction Center. Retrieved 2007-05-10.
  17. ^ a b c Canadian Hurricane Center (2007). "2006 Tropical Cyclone Season Summary". Retrieved 2007-05-10.
  18. ^ a b c d Bowyer & Roussel (2006). "Tropical Storm Alberto Information Statement for June 15, 2006 (2)". Canadian Hurricane Centre. Retrieved 2007-05-10.
  19. ^ a b Roussel & Marshall (2006). "Tropical Storm Alberto Information Statement for June 16, 2006". Canadian Hurricane Centre. Retrieved 2007-05-10.
  20. ^ a b c Dalia Acosta (2006-06-15). "Tempestade tropical Alberto causa estragos; Cuba: Os estragos causados por Alberto" (in Portuguese). Inter Press Service. {{cite news}}: |access-date= requires |url= (help)
  21. ^ a b Agence France-Presse (2006-06-12). "25,000 Cubans move from 'life-threatening' storm Alberto". Retrieved 2008-02-12.
  22. ^ a b Knabb (2006). "Tropical Depression One Public Advisory Two". National Hurricane Center. Retrieved 2007-05-10.
  23. ^ "20,000 ordered to leave Florida's Gulf Coast". Associated Press. June 12, 2006. Retrieved 2006-06-13. {{cite news}}: Check date values in: |date= (help)
  24. ^ "Hernando County issues a recommended evacuation of Zone A/B". WTSP. June 12, 2006. Retrieved 2006-06-12. {{cite news}}: Check date values in: |date= (help)
  25. ^ a b c d National Climatic Data Center (2006). "Event Report for Florida (3)". Retrieved 2007-05-21.
  26. ^ Bush, Jeb (2006). "Executive Order Number 06-130- Tropical Storm Alberto" (PDF). Retrieved 2006-06-12.
  27. ^ LaFortune (2006). "Tropical Storm Alberto Information Statement for June 14, 2006". Canadian Hurricane Centre. Retrieved 2007-05-10.
  28. ^ LaFortune & Bowyer (2006). "Tropical Storm Alberto Information Statement for June 15, 2006". Canadian Hurricane Centre. Retrieved 2007-05-10.
  29. ^ LaFortune & Bowyer (2006). "Tropical Storm Alberto Information Statement for June 14, 2006 (2)". Canadian Hurricane Centre. Retrieved 2007-05-10.
  30. ^ Cuban delegates to the World Meteorological Organization (2007). "Reports of hurricanes, tropical storms, tropical disturbances and related flooding during 2006 in Cuba" (PDF). Retrieved 2007-05-10.
  31. ^ Alberto Hernández Unzón (2006). "Resumen de la Tormenta Tropical "Alberto" del Océano Atlántico" (PDF). Servicio Meteorológico Nacional. Retrieved 2007-05-11.
  32. ^ National Climatic Data Center (2006). "Event Report for Florida". Retrieved 2007-05-21.
  33. ^ Tallahassee, Florida National Weather Service (2006). "Tropical Storm Alberto 2006". NOAA. Retrieved 2007-05-21.
  34. ^ a b National Climatic Data Center (2006). "Event Report for Florida (2)". Retrieved 2007-05-21.
  35. ^ National Climatic Data Center (2006). "Event Report for Florida (4)". Retrieved 2007-05-21.
  36. ^ Associated Press (2006). "Coast Guard ends search for 'missing' boaters". Retrieved 2007-05-21.
  37. ^ Leon Fooksman (2006). "Possible sinking-boat hoax cost $278,000 for daylong air and sea search". South Florida Sun-Sentinel. Retrieved 2007-05-21.
  38. ^ The United States Attorney's Office (2006). "Boynton Beach Man Sentenced to Prison for Making Hoax Distress Call to the Coast Guard". Retrieved 2007-05-21.
  39. ^ National Climatic Data Center (2006). "Event Report for Georgia". Retrieved 2007-05-18.
  40. ^ a b Charleston, South Carolina National Weather Service (2006). "Tropical Storm Alberto Post Tropical Cyclone Report". NOAA. Retrieved 2007-05-18.
  41. ^ Blaes (2006). "Remnants of Alberto Produced Record Rainfall Amounts Across Central North Carolina". Raleigh, North Carolina National Weather Service. Retrieved 2007-05-20.
  42. ^ Raleigh, NC National Weather Service (2006). "Tropical Storm Alberto Event Summary". Retrieved 2007-05-20.
  43. ^ ABC11TV (2006). "Alberto Brings Worst Flooding Since Fran". Retrieved 2007-05-20.{{cite web}}: CS1 maint: numeric names: authors list (link)
  44. ^ National Climatic Data Center (2006). "Event Report for North Carolina". Retrieved 2008-02-12.
  45. ^ Cullen (2006). "Tropical Storm Alberto Post-Storm Report". Wakefield, Virginia National Weather Service. Retrieved 2007-05-20.
  46. ^ National Climatic Data Center (2006). "Event Report for Virginia". Retrieved 2007-05-20.
  47. ^ Bowyer (2006). "Tropical Storm Alberto Information Statement for June 14, 2006 (3)". Canadian Hurricane Centre. Retrieved 2007-05-10.
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