The rising air is loaded with water vapor. As it shoots into the colder upper atmosphere, the vapor condenses into a skyscraper of a cloud: the cumulonimbus. In less than 30 minutes, a clear blue sky turns into a dark, purple-gray ceiling. The wind dies, then returns in a gust. The temperature drops 15 degrees.
Nature abhors a vacuum. So, the cool ocean air races inland to fill the void left by the rising hot air. By early afternoon, two invisible armies of wind—the from the east and the Gulf sea breeze from the west—march across the peninsula. The Climax: The 3 P.M. Collision This is the moment everyone in Florida knows by heart. when is the rainy season in florida
Between 2 p.m. and 4 p.m., the two sea breezes collide in the middle of the state, often right over Interstate 4, which runs from Tampa to Daytona Beach. This is known as the . When these two walls of moist, unstable air smash into each other, they have nowhere to go but up . The rising air is loaded with water vapor