Convection in the atmosphere is mainly the result of the fact that more of the Sun's heat energy is received by parts of the Earth near the Equator than at the poles.
(Convection in the atmosphere; is mainly; the result of the fact that more of the Sun's heat energy is received by parts of the Earth near the Equator than at the poles) (more of the Sun's heat energy; is received; by parts of the Earth; L:near the Equator)
Convection in the atmosphere more of the Sun's heat energy
is mainly is received
the result of the fact that more of the Sun's heat energy is received by parts of the Earth near the Equator than at the poles
by parts of the Earth L:near the Equator