Abstract
The purpose of this paper is to investigate the influence of cloudiness on the shortwave radiation budget at the top of the atmosphere, at the surface, and as a residual, for the atmosphere itself. The data used for this study are derived exclusively from satellite measurements. The concept of cloud radiative forcing is applied to these different datasets. It is shown that the solar cloud forcing at the top of the atmosphere (CFTOA), and at the surface (CFSUR), are of the same order of magnitude and well correlated with cloud cover (R = 0.83). On the contrary, the solar cloud forcing of the atmosphere itself, CFATM, is about one order of magnitude less and not very highly correlated with cloud cover (R=0.37). The mean value of the annual averaged solar cloud forcing for the area of investigation is calculated for the top of the atmosphere to be CFTOA = 50 ± 4 W m-2, for the surface to be CFSUR = 55 ± 6 W m-2, and for the atmosphere to be CFATM = -5 ± 10 W m-2. Related to the annual mean solar insolation, the CFATM corresponds to an additional contribution of the clouds to atmospheric solar absorption of 1.4%. -from Authors
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CITATION STYLE
Rieland, M., & Stuhlmann, R. (1993). Toward the influence of clouds on the shortwave radiation budget of the earth-atmosphere system estimated from satellite data. Journal of Applied Meteorology, 32(5), 825–843. https://doi.org/10.1175/1520-0450(1993)032<0825:TTIOCO>2.0.CO;2
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