It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
the equator warm and humid
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
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.
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.
The Amazon is hot and humid due to its location. It is near the equator where the sun's rays are known to be more direct causing the immense heat. The humidity is contributed to the water in the air being heated. As the sun's rays are heating the Earth, the water in the air rises as well causing the humidity to rise in the Amazon.
the equator warm and humid
It cools and consequently can hold less water vapour. The vapour condenses and it rains. This is convection rainfall.
Africa
Because Europe is not located near 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.
in countries near the equator in Africa and south america
in countries near the equator in Africa and south america
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.
in countries near the equator in Africa and south america
dsadas
Mosty hot and humid as it lies within the tropics
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.