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You get less evaporation, less moisture in the atmosphere, and less rainfall again.
Not exact matches
... the higher up you go the
less water vapor you normally
get because it is too cold to have available water vapor (the rate of condensation strongly exceeds the rate of
evaporation)... unless you warm it and «suddenly water vapor just appears» where it was mostly absent before.
Though one could
get more clouds in temperate and polar regions if there
less clouds in tropics - generating massive amount of
evaporation.
Because the sea surface
gets colder, there is
less evaporation, and thus
less heat transfer from the ocean to the atmosphere during the time it takes for the water to reach the Arctic Ocean.
If drought makes soils dryer, there will be
less evaporation — and thus the surface will
get hotter.