Tropical cyclone

From WikiMD.org
Jump to navigation Jump to search

Tropical cyclone

A Tropical cyclone (pronunciation: /ˈtrɒpɪkəl ˈsaɪkləʊn/) is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and, in some cases, tornadoes.

Etymology

The term "Tropical cyclone" is derived from the word "tropical", which refers to the geographical origin of these systems, which form almost exclusively over tropical seas, and "cyclone", from the Greek "κυκλών", meaning "whirling, moving in a circle".

Related terms

  • Tropical depression: A tropical cyclone with maximum sustained winds of 38 mph (33 knots) or less.
  • Tropical storm: A tropical cyclone with maximum sustained winds of 39 to 73 mph (34 to 63 knots).
  • Hurricane: A tropical cyclone with maximum sustained winds of 74 mph (64 knots) or more.
  • Typhoon: A mature tropical cyclone that develops in the western part of the North Pacific Ocean.
  • Cyclone: A large scale air mass that rotates around a strong center of low atmospheric pressure.
  • Storm surge: A rise in sea level that occurs during tropical cyclones, significantly increasing the potential for coastal flooding.

See also

External links

Esculaap.svg

This WikiMD dictionary article is a stub. You can help make it a full article.


Languages: - East Asian 中文, 日本, 한국어, South Asian हिन्दी, Urdu, বাংলা, తెలుగు, தமிழ், ಕನ್ನಡ,
Southeast Asian Indonesian, Vietnamese, Thai, မြန်မာဘာသာ, European español, Deutsch, français, русский, português do Brasil, Italian, polski