Input is received in the form of short-wave solar energy. This is called insolation. Only approximately 52 per cent of this insolation reaches the earth's surface. The rest is absorbed by water ...
Berger, A. & Loutre, M. F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297-317 (1991). CAPE Project Members. Holocene paleoclimate data from the ...
In this region, incoming insolation exceeds outgoing radiation. There's an energy deficit between 35Ëš North and the North Pole, and between 35Ëš South and the South Pole. Here the outgoing ...
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