Tropical cyclones form over warm ocean waters with surface temperatures above 26°C. As warm air rises from the ocean surface, it creates a low pressure area at the center. Surrounding winds begin to rotate inward due to the Coriolis effect from the Earth's rotation. Thunderstorms form in a spiral pattern around the low pressure center, and if conditions continue to allow for further development, a tropical cyclone will form. Once over land, tropical cyclones weaken due to a lack of warm ocean waters providing energy and moisture.