A tropical cyclone 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 rains and potentially dangerous storm surges. Tropical cyclones are known by different names in different regions of the world, such as hurricanes, typhoons, or cyclones.
Tropical cyclones typically form over warm ocean waters near the equator. The warm water provides the energy and moisture needed for the storm to develop and strengthen. As the warm, moist air rises, it creates an area of low pressure at the surface, which draws in more air and causes the storm to rotate. The Earth's rotation then causes the storm to spin, and as it gains strength, it can develop into a tropical cyclone.
A tropical cyclone is characterized by a well-defined center called the "eye," surrounded by bands of thunderstorms and strong winds. The eyewall, located around the eye, is where the most intense winds and rain occur. The storm's outer rainbands can also produce heavy rainfall and strong winds. Tropical cyclones are categorized by their wind speeds, with the Saffir-Simpson Hurricane Wind Scale used in the Atlantic and Eastern Pacific, and the Typhoon Classification System used in the Western Pacific.
Tropical cyclones can have significant impacts, including strong winds, heavy rainfall, storm surges, and flooding. These storms can cause widespread damage to infrastructure, homes, and agriculture, and can also result in loss of life. Coastal regions are particularly vulnerable to storm surges, which can inundate coastal areas and cause extensive flooding. Preparedness and early warning systems are important for minimizing the impacts of tropical cyclones.