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It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.

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Jerrold Quitzon

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3y ago

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Related Questions

What is near the pole s and equator?

the equator warm and humid


What happens after hot humid air near the equate rises?

It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.


What are places near the equator that have Humid Tropical climents?

Africa


Why is there no humid tropical climate in Europe?

Because Europe is not located near the equator.


What happens when the equator receives more of the sun's energy?

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.


Where are humid tropicals?

in countries near the equator in Africa and south america


Where are humid tropical climates found?

in countries near the equator in Africa and south america


What happens to the air at the equator?

At the equator, warm air rises due to intense heating, creating a low-pressure zone. As the air rises, it cools, condenses, and produces heavy rainfall. This process contributes to the formation of tropical rainforests near the equator.


Where are humid tropical climates?

in countries near the equator in Africa and south america


Where are' calm areas near the equator where warm air rises are?

dsadas


What is the climate of Africa near the equator?

Mosty hot and humid as it lies within the tropics


What happend after hot humid air near the equator rises?

After hot, humid air near the equator rises, it cools at higher altitudes, leading to condensation and the formation of clouds. This process often results in precipitation, contributing to tropical rainforests' lush ecosystems. The rising air creates a low-pressure area, which draws in more warm, moist air from surrounding regions, perpetuating the cycle of convection and storm development. This phenomenon is also a key component of the Hadley cell circulation in Earth's atmosphere.