Abstract
Tropical cyclones—the generic name for intense, rotating vortices of air that sustain themselves on the energy that is released when water condenses in clouds—are known by different names in different parts of the world, including hurricanes, typhoons, and cyclones. This chapter describes the energy transformations that occur in tropical cyclones and how these transformations result in such destructive weather systems. The environmental conditions necessary for the development of tropical cyclones are then described, along with the Saffir-Simpson scale, which is used to categorize tropical cyclones by strength. Composite maps of global tropical cyclone tracks, by month, during the “Satellite Era” and for the longer period of instrumental observation reveal the climatology of conditions suitable for these storms. Finally, the types of damage and impacts caused by these significant weather systems in coastal areas are described. These include strong winds, tornadoes, mergers with extratropical frontal systems, flooding, and storm surges.
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