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・ Tropical cyclone
・ Tropical cyclone basins
・ Tropical cyclone effects in Europe
・ Tropical Cyclone Evan
・ Tropical cyclone forecast model
・ Tropical cyclone forecasting
・ Tropical Cyclone Formation Alert
・ Tropical cyclone naming
・ Tropical cyclone observation
・ Tropical cyclone rainfall climatology
・ Tropical cyclone rainfall forecasting
・ Tropical cyclone scales
・ Tropical cyclone seasonal forecasting
・ Tropical cyclone track forecasting
・ Tropical cyclone warnings and watches
Tropical cyclone windspeed climatology
・ Tropical cyclones and tornadoes in Pakistan
・ Tropical cyclones in 2005
・ Tropical cyclones in 2006
・ Tropical cyclones in 2007
・ Tropical cyclones in 2010
・ Tropical cyclones in popular culture
・ Tropical Dandy
・ Tropical Depression (band)
・ Tropical Depression (EP)
・ Tropical Depression 01W
・ Tropical Depression 02W
・ Tropical Depression 03W
・ Tropical Depression 04F (2009)
・ Tropical Depression 04W


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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.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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