The vertical height reached by convective currents in the atmosphere is called:

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The vertical height reached by convective currents in the atmosphere is called the mixing depth. It is the maximum height reached by convective currents during the day and is influenced by factors such as solar radiation, wind speed, and surface characteristics. The convective inversion refers to the layer of atmosphere where temperature increases with height, which can inhibit convective mixing. Vertical transport potential refers to the ability of atmospheric motions to transport pollutants or other substances vertically in the atmosphere. A temperature inversion is a situation where temperature increases with height, which can also inhibit convective mixing.

The Vertical Height Reached by Convective Currents in the Atmosphere