The net effect of circulation is to move warm air from the
and thus moderate the equator-to-pole energy gradient created by .
(a) the tropics to the poles; the difference insolation absorbed in day and night
(b) the tropics to the poles; ocean circulation
(c) from the surface up to the tropopause; more heating near the ground than
aloft
(d) the tropics to the poles; the latitudinal distribution of absorbed
insolation
(e) from the surface up to the tropopause; more heating in the atmosphere than
at the surface from GHGs
and thus moderate the equator-to-pole energy gradient created by .
(a) the tropics to the poles; the difference insolation absorbed in day and night
(b) the tropics to the poles; ocean circulation
(c) from the surface up to the tropopause; more heating near the ground than
aloft
(d) the tropics to the poles; the latitudinal distribution of absorbed
insolation
(e) from the surface up to the tropopause; more heating in the atmosphere than
at the surface from GHGs