Meteosat data as an index of fluctuations in Earth radiation budget on weekly and monthly time scales.
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Abstract
Studies of the overall themodynamic and "chaotic" behaviour (Ruelle, 1985) of thr Earth-atmosphere climate system require long time-series of the total solar radiation absorbed by the system and of the total infrared radiation emitted by system. The series should extend several years in order to examine fluctuations of net energy input on time scales of several days to several months.
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