A globally averaged, one-dimensional radiative-convective climate model is used to study the effect of clouds on both the climate and the sensitivity of climate to changes in incoming solar radiation. The model has been run with low, mid and high clouds of different areas, heights and liquid water contents. -from Author
CITATION STYLE
Charlock, T. P. (1982). Cloud optical feedback and climate stability in a radiative- convective model. Tellus, 34(3), 245–254. https://doi.org/10.3402/tellusa.v34i3.10808
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