A tropical cyclone is a storm system
characterized by a large low-pressure center and numerous thunderstorms that produce strong winds and heavy rain. Tropical cyclones strengthen when
water evaporated from the ocean is
released as the saturated air rises,
resulting in condensation of water
vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic
windstorms such as nor'easters,
European windstorms, and polar lows. The characteristic that separates tropical cyclones from other cyclonicsystems is that at any height in the atmosphere, the center of a tropical
cyclone will be warmer than its
surroundings; a phenomenon called "warm core" storm systems. Depending on its location and
strength, a tropical cyclone is referred to by names such as hurricane, typhoon, tropical storm, cyclonic storm, tropical depression, and simply cyclone. A tropical storm is an organized system of strong thunderstorms with a
defined surface circulation and
maximum sustained winds between
17-32 metres per second.
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