Nonradiative heat transfer again compensates for the imbalance, this time largely by vertical atmospheric motions involving the evaporation and condensation of water.
Not exact matches
A balance is established through
nonradiative processes, namely conduction and convection, that
heat the atmosphere.
Other
nonradiative forcings modify the biological components of the climate system by changing the fluxes of trace gases and
heat between vegetation, soils, and the atmosphere and by modifying the amount and types of vegetation.
The atmosphere and oceans, through their general circulation, act as vast
heat engines, compensating for this imbalance by providing
nonradiative mechanisms for the transfer of
heat from the Equator to the poles.
Another important
nonradiative mechanism is the exchange of
heat that occurs when the temperature of the air is different from that of the surface.