Tropical cyclone windspeed climatology information
Wind Swath of Hurricane King over Miami
Tropical cyclone windspeed climatology is the study of wind distribution among tropical cyclones, a significant threat to land and people. Since records began in 1851, winds from hurricanes, typhoons and cyclones have been responsible for fatalities and damage in every basin. Major hurricanes (Category 3 or above) usually cause the most wind damage.[1] Hurricane Andrew for example caused $45 billion(2005 USD) in damage, most of it wind damage.[2]
Although wind damage is rare to tropical cyclones near landmasses, there are a few factors that lead to high wind speeds. Warm water temperatures, which was seen during Hurricane Wilma when its winds rapidly strengthened to 185 mph (298 km/h) in a 24-hour period due to the presence of abnormally warm water temperatures. Size and speed of the storm, which results in damage along a wide area as seen in Hurricane Isabel and Great New England Hurricane of 1938.[3][4]
^"TCFAQ D1) How are Atlantic hurricanes ranked?". Aoml.noaa.gov. Retrieved 7 May 2014.
^NHC Report on Andrew
^Hurricane Wilma Report
^Hurricane Isabel Report
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