Insolation,the energy input for the climate system,is largely determined by

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Insolation, or the amount of solar radiation received by the Earth's surface, is largely determined by latitude. This is because the angle of the sun's rays changes with latitude, with areas closer to the equator receiving more direct sunlight and areas closer to the poles receiving more indirect sunlight. Altitude, high pressure cells, upper atmospheric circulation, and local and regional winds can also affect insolation, but their impact is generally secondary to latitude.

Insolation,the Energy Input for the Climate System,is Largely Determined by