Respuesta :
tectonic forces influence mass movement in all of the following ways except: controls the amount of rainfall an area receives.
Factors controlling the dissemination of rainfall over the world's surface are the belts of merging climbing wind stream (see dejection; polar front), air temperature, moisture-bearing breezes, sea ebbs and flows, distance inland from the coast, and mountain ranges.
Rising air is cooled by extension, which brings about the development of mists and the creation of downpour. Alternately, in the expansive belts of sliding air (see horse latitudes) are found the extraordinary desert locales of the earth, slipping air being warmed by pressure and thusly retaining as opposed to delivering moisture. On the off chance that the temperature is low, the air has a little moisture limit and can deliver little precipitation.
At the point when winds blow over the sea, particularly over areas of warm water (where vanishing of moisture high up is dynamic) toward a given beach front region, that region gets more rainfall than a comparable region where the breezes blow from the inside toward the seas. Regions close to the ocean get more downpour than inland districts, since the breezes continually lose moisture and might be very dry when they arrive at the inside of a landmass.
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tectonic forces influence mass movement in all of the following ways except: controls the amount of rainfall an area receives.
Factors controlling the dissemination of rainfall over the world's surface are the belts of merging climbing wind stream (see dejection; polar front), air temperature, moisture-bearing breezes, sea ebbs and flows, distance inland from the coast, and mountain ranges.
Rising air is cooled by extension, which brings about the development of mists and the creation of downpour. Alternately, in the expansive belts of sliding air (see horse latitudes) are found the extraordinary desert locales of the earth, slipping air being warmed by pressure and thusly retaining as opposed to delivering moisture. On the off chance that the temperature is low, the air has a little moisture limit and can deliver little precipitation.
At the point when winds blow over the sea, particularly over areas of warm water (where vanishing of moisture high up is dynamic) toward a given beach front region, that region gets more rainfall than a comparable region where the breezes blow from the inside toward the seas. Regions close to the ocean get more downpour than inland districts, since the breezes continually lose moisture and might be very dry when they arrive at the inside of a landmass.
to know more about the horse latitude click here:
brainly.com/question/27966282
#SPJ4
