High sea temperatures causes warm air from convection currents to rise, simultaneously causing a build up of energy and low pressure. This energy results in the powerful kinetic energy within a cyclone (with the help of latent heat.) The Coriolis effect then causes the cyclone to spin, as it is also the most energy stabilized way of movement
the warm air doesn't come *from* the convection currents, but *causes* a convection current. warm air rises, and cools in the upper atmosphere, then falls. Can you try explaining it again.
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