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Tropical cyclone windspeed climatology : ウィキペディア英語版 | Tropical cyclone windspeed climatology
A significant threat from tropical cyclones is high winds. 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. Hurricane Andrew for example caused $45 billion (2005 USD) in damage, most of it wind damage.〔(NHC Report on Andrew )〕 Although wind damage is common 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 it winds rapidly strengthened to 185 mph (295 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.〔(Hurricane Wilma Report )〕〔(Hurricane Isabel Report )〕 ==Winds in tropical cyclones== (詳細はevaporation and condensation of moisture which results in updrafts. The updrafts in turn increase the height of the storm which causes more condensation.
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