What happens to the air over land during a wet monsoon?

During a wet monsoon, the air over land typically rises due to intense convection. This phenomenon occurs because the land heats up more quickly than the surrounding water. As the temperature of the air above the land increases, it becomes less dense and starts to rise. The warm, moist air rises and cools at higher altitudes, leading to the formation of clouds and precipitation. This convective process is a key characteristic of monsoonal weather patterns, where the energy from the sun drives the rising motion of warm, moist air, resulting in heavy rainfall often associated with these seasons.

In contrast, during a wet monsoon, the air does not cool down rapidly or remain stagnant; instead, its dynamic nature is marked by rising warm air and subsequent cooling. The dispersal of air towards the ocean is not a primary characteristic of a wet monsoon, as the focus is on the rising air and precipitation over land.