The vertical height reached by convective currents in the atmosphere is called:
A) a temperature inversion.
B) the mixing depth.
C) vertical transport potential.
D) the convective inversion.

Question

Quizplus · Accepted Answer

The mixing depth refers to the vertical height that convective currents can reach in the atmosphere, influenced by factors such as temperature, humidity, and atmospheric stability.

The Vertical Height Reached by Convective Currents in the Atmosphere