The region of greatest solar heating at the surface in the humid tropics corresponds to areas of deep
cumulonimbus convection.
Not exact matches
The intertropical convergence zone is distinguished by a wide band of cumulus and
cumulonimbus clouds that are created by dynamic atmospheric lifting due to convergence and
convection.
The warm water evaporates from the ocean surface, and the light, warm and humid air rises, leading to deep
convection in the form of towering
cumulonimbus clouds and heavy precipitation.