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・ Tropical Brainstorm
・ Tropical Campfires
・ Tropical climate
・ Tropical conger
・ Tropical crabgrass
・ Tropical cyclogenesis
・ 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)


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Tropical cyclone rainfall climatology : ウィキペディア英語版
Tropical cyclone rainfall climatology

A tropical cyclone rainfall climatology is developed to determine rainfall characteristics of past tropical cyclones. A tropical cyclone rainfall climatology can be used to help forecast current or upcoming tropical cyclone impacts. The degree of a tropical cyclone rainfall impact depends upon speed of movement, storm size, and degree of vertical wind shear. One of the most significant threats from tropical cyclones is heavy rainfall. Large, slow moving, and non-sheared tropical cyclones produce the heaviest rains. The intensity of a tropical cyclone appears to have little bearing on its potential for rainfall over land, but satellite measurements over the last several years show that more intense tropical cyclones produce noticeably more rainfall over water. Flooding from tropical cyclones remains a significant cause of fatalities, particularly in low-lying areas.
==Anticipating a flood event==

While inland flooding is common to tropical cyclones, there are factors which lead to excessive rainfall from tropical cyclones. Slow motion, as was seen during Hurricane Danny (1997) and Hurricane Wilma, can lead to high amounts of rainfall. The presence of mountains/hills near the coast, like across much of Mexico, Haiti, the Dominican Republic, Central America, Madagascar, Réunion, China, and Japan acts to magnify rainfall potential due to forced upslope flow into the mountains. Strong upper level forcing from a trough moving through the Westerlies and its associated cold front, as was the case during Hurricane Floyd, can lead to high amounts even from systems moving at an average forward motion. Larger tropical cyclones drop more rainfall as they precipitate upon one spot for a longer time frame than average or small tropical cyclones. A combination of two of these factors could be especially crippling, as was seen during Hurricane Mitch in Central America. During the 2005 season, flooding related to slow-moving Hurricane Stan's broad circulation led to 1,662–2,000 deaths.〔"(Dennis, Katrina, Rita, Stan, and Wilma "Retired" from List of Storm Names )." ''NOAA.'' Retrieved on June 14, 2008.〕

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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