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Shortwave radiation penetrates a volume of water to significant depths (up to several hundred metres) before the insolation is completely attenuated.
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Blackwelder, E. The insolation hypothesis of rock weathering.
Comparison of b with c reveals that the insolation peak that triggered deglaciation was only as large as other insolation peaks that did not induce deglaciation.
Laskar, J. et al. A long-term numerical solution for the insolation quantities of the Earth.
The insolation readings were not compared with a calibrated pyranometer, but were reasonable for the light levels experienced.
Consequently, the extracted power increases exponentially with the insolation.
One way in which the insolation is affected is by the clouds.
Opposite to the insolation effects, the temperature has a drastic impact on the solar cell efficiency.
So the rainfall over the IMC is sensitive to the insolation.
As shown, the insolation reaching south-facing walls were relatively small, but not inconsequential.
The insolation is thus defined by the following equation: I = I 0 ∗ exp − AM ∗ τ (5).
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