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What is the impact of coriolls force and latent on the development of tropical cyclone​

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Coriolis force is a phenomenon arising from the Earth's rotation. In the Northern Hemisphere, this force deflects objects to the right. In theSouthern Hemisphere, it deflects them to the left. This force can affect the motion of air in the atmosphere, including the movement of air around tropical cyclones. As a result, the Coriolis force initiates the rotation of tropical cyclones necessary for their development.

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Latent heat is the energy released or absorbed when water changes phase, such as when water vapor condenses into liquid. In the context of tropical cyclones, latent heat is released when water vapor condenses into cloud droplets and raindrops. This helps fuel the storm's development and intensification. As moist air rises and cools, water vapor condenses, releasing latent heat that provides additional energy to the storm.

Together, these two factors influence the development and intensification of tropical cyclones. The Coriolis force initiates the rotation of tropical cyclones, while latent heat provides the energy needed to fuel their development and intensification. Without these factors, tropical cyclones may not form or maintain their strength.

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