It rises creating a low pressure region near the ground
Air Equator was created in 2003.
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
Clouds form as air rises at the equator.
It often rains around the Equator because this region gets a lot of sunlight, which heats the air. Warm air rises and cools as it goes higher, causing moisture to condense and form clouds. When the clouds get heavy enough, they release rain. This process happens almost daily, leading to frequent rain in tropical areas near the Equator.
Nothing happens at the equator that does not happen elsewhere.
Nothing happens at the equator that does not happen elsewhere.
Air Equator ended in 2005.
Air Equator was created in 2003.
Clouds form as air rises at the equator.
When the equator receives more of the sun's energy, it experiences warmer temperatures, resulting in hotter and more humid climates. This can lead to the formation of tropical rainforests near the equator due to the increased warmth and moisture.
The Coriolis effect causes an air mass moving from the North Pole to the equator to bend to the west, or turn toward the right. In the Southern Hemisphere the opposite happens.
Warm air rises at the equator and cold air sinks at the poles. Warm air expands and cool air contracts and compresses.
Clouds form as air rises at the equator.
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
The air around the equator is caught in the doldrums and the trade winds. The air closest to the equator flows upward and westerly until it reaches the border of the prevailing westerlies when it heads back toward the equator again.
It often rains around the Equator because this region gets a lot of sunlight, which heats the air. Warm air rises and cools as it goes higher, causing moisture to condense and form clouds. When the clouds get heavy enough, they release rain. This process happens almost daily, leading to frequent rain in tropical areas near the Equator.