The primary source of energy for all tropical cyclones is warm ocean water. Tropical cyclones, also known as hurricanes or typhoons in different regions, form over warm sea surfaces, typically when sea surface temperatures exceed about 26 degrees Celsius (79 degrees Fahrenheit). The warm water heats the air above it, causing it to rise, which in turn creates a low-pressure area. This process leads to the evaporation of water from the ocean surface, which adds moisture to the atmosphere. As the warm, moist air rises, it cools and condenses, releasing latent heat that further fuels the storm and enhances its development. Additionally, tropical cyclones require specific atmospheric conditions, such as low wind shear and sufficient Coriolis force, but the underlying energy primarily comes from the ocean's warmth.
What is the source of energy for all tropical cyclones
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