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Tropical Storm Claudette (2009)

Tropical Storm Claudette
Tropical storm (SSHWS/NWS)
Claudette 2009 approaching Florida.jpg
Tropical Storm Claudette intensifying off the Florida coast on August 16
Formed August 16, 2009
Dissipated August 18, 2009
Highest winds 1-minute sustained: 60 mph (95 km/h)
Lowest pressure 1005 mbar (hPa); 29.68 inHg
Fatalities 2 direct
Damage $228,000 (2009 USD)
Areas affected Southeastern United States
Part of the 2009 Atlantic hurricane season

Tropical Storm Claudette was the third named storm of the 2009 Atlantic hurricane season and the first tropical cyclone of 2009 to affect the United States. Forming out of a tropical wave and an upper-level low pressure system on August 16, Claudette quickly intensified into a tropical storm offshore south of Tallahassee, Florida. By the afternoon, the storm had attained winds of 60 mph (95 km/h) and steadily tracked towards the Florida Panhandle. Early on August 17, the center of Claudette made landfall on Santa Rosa Island. Several hours after landfall, the storm weakened to a tropical depression and the Hydrometeorological Prediction Center took over primary responsibility of the storm. Later on August 17, the final public advisory was issued on the system as it dissipated over Alabama.

The National Hurricane Center issued tropical storm warnings for the coastline and residents in some counties were advised to evacuate storm-surge-prone areas. One fatality resulted from rough seas off the coast of Panama City, Florida. Later that day, another man drowned after falling off his ship near Bay County. An EF-0 tornado spawned by the storm in Cape Coral, Florida damaged 11 homes, leaving $103,000 (2009 USD) in damages. Additional damages to coastal property and beaches amounted to $125,000 (2009 USD) as a result of Claudette.

Tropical Storm Claudette originated from a tropical wave that moved off the west coast of Africa on August 7. On August 11, the National Hurricane Center (NHC) began monitoring the wave when it was located roughly 600 mi (965 km) east of the Lesser Antilles. Disorganized shower and thunderstorm activity was associated with the westward moving wave; however, the NHC did not anticipate further development of the system. By the afternoon of August 12, little convective activity remained with the wave. Strong upper-level wind shear created an unfavorable environment for the system to re-organize as it tracked through the eastern Caribbean Sea.


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