Parameterization of the radiative flux divergence in the 9.6 micron O3 band

Physics

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Atmospheric Temperature, Cooling, Flux Quantization, Oxygen Spectra, Ozone, Radiative Transfer, Absorbers (Materials), Parameterization, Rates (Per Time), Spectral Bands

Scientific paper

A parameterization of the cooling rate of the earth's atmosphere in the height region of approximately 20-75 km due to radiation transfer in the 9.6 micron O3 band is proposed. A general random band model is used to calculate the radiation transmission. The parameterization takes into consideration a peculiar feature of the radiative transfer - the height step increases with growing distance from the level for which cooling is calculated. A simple method of accounting for the variation of the vertical profile of the absorbing gas is proposed and utilized. The procedure proposed is multiparametric; 22 parameters are prescribed for calculating cooling at a given level. The procedure can be recommended for calculating radiative cooling for any temperature and ozone profile not having a small- or mesoscale structure. It can be used, in particular, for modeling of the middle atmospheric circulation.

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