Titlebook: Radiation in a Cloudy Atmosphere; E. M. Feigelson Book 1984 D. Reidel Publishing Company, Dordrecht, Holland 1984 Absorption.Aerosol.Albed

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Methods of Calculating Thermal Radiation2, 24], and in a number of collections and original articles. In this chapter we will present only some of the initial relations and we will describe some of the approximate calculation methods used in practice.

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Introductionified initial moment can the dynamic processes in the atmosphere be considered to be adiabatic. Global dynamic processes of long duration are regulated by the actual influxes of heat, one of the main ones being the radiative influx.

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Physical Characteristics of Cloudsever, the temperature fluctuations may be considerable, reaching 1 to 3°C. On the average, these clouds stay a little (0.2-0.5°C) cooler than the ambient air [9]. Inside the clouds the temperature gradients are, as a rule, close to moist-adiabatic.