Tropical Cyclone

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A storm system characterised by a large low-pressure centre and thunderstorms that produce strong winds and heavy rain. More technically, it is a non-frontal synoptic scale cyclone originating over tropical or sub-tropical waters with organised convection and definite cyclonic surface wind circulation
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Topography is considered when a tropical cyclone develops nearby, or passes over landmass during its track [2], cutting the storm off from the ocean-surface and disrupting the OIA.
pot] is the potential intensity (the theoretical maximum intensity a tropical cyclone can reach in a given thermodynamic environment), [C.
If an area of low pressure develops within the leading edge of the monsoon rains, then occasionally it can develop into a tropical cyclone.
It depends completely on the movement of this tropical cyclone.
According to the study, the latitude at which tropical cyclones reach their greatest intensity is gradually shifting from the tropics toward the poles at rates of about 33 to 39 miles per decade.
For further information on tropical cyclone warnings in the South Pacific region, please consult the Joint Typhoon Warning Center in Honolulu and the National Weather Service's Central Pacific Hurricane Center, Fiji's regional meteorological center responsible for tropical cyclone warnings in the South Pacific region, or the Government of Australia's Bureau of Meteorology.
Their paper, "The Track Integrated Kinetic Energy of the Atlantic Tropical Cyclones," was published in the American Meteorological Society's Monthly Weather Review.
During the last 50 years three very wet tropical cyclone events -- Typhoons Morakot, Herb and Flossie -- were followed within four years by major earthquakes in Taiwan's mountainous regions.
by the tropical Cyclone Phet that hardly hit most of the Sultanate of Oman in
It would turn into a moderate intensity tropical cyclone with maximum sustained wind of about 70-90 kilometres per hour with the associated storm surge of 3-5 metres.
Guy Carpenter's Instrat unit has issued reports about last year's notable global tropical cyclone activity as well as 2008 manmade and technical catastrophes.
The principal result is that regions favorable to the development of tropical cyclone development are characterized by strong negative spatial gradients of evaporation with respect to SST, whereas cyclones are likely to be spun-down in regions of strong positive gradients.

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