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The fuel for a tropical cyclone is provided by a transfer of water vapour and heat from the warm ocean to the overlying air, primarily by evaporation from the sea surface. As the warm, moist air rises, it expands and cools, quickly becoming saturated and releasing latent heat through the condensation of water vapour.
In the western Pacific they are called typhoons, while in the eastern Pacific and Atlantic Oceans they are called hurricanes. Typhoon and Hurricanes form in the exact same way, they get their energy from warm tropical water in the Pacific and Atlantic oceans.
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