The ocean's warm surface is cooled by strong upward movement of air, forming towering thunderstorm clouds. The Coriolis force powers these clouds, releasing heat and drawing more water from the ocean. As surface winds reach 120km/h, the storm becomes a tropical storm. It develops an eye at its center, with intense weather conditions felt in the outer eye. As it reaches land, the storm's energy supply is cut off, slowing it down and weakening. However, if it reaches warm seas, it may regain strength.