Physics
Scientific paper
Jan 1997
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997jqsrt..57....1z&link_type=abstract
Journal of Quantitative Spectroscopy and Radiative Transfer, vol. 57, issue 1, pp. 1-10
Physics
Earth Atmosphere: Radiative Transfer, Earth Atmosphere: Thermal Properties, Earth Atmosphere: Transmission
Scientific paper
Mechanisms of the influence of the atmospheric transmission function, in the range 2-400 μm and especially in the windows 8-13 and 3-4 μm, on the thermal balance of the Earth's atmosphere are discussed. The negative and positive feedbacks between the absorption of the outgoing heat radiation in the atmosphere and the heating of the Earth's surface are considered. The database GEISA-92, which provides spectral line parameters of atmospheric constituents, has been used for simulations of infrared radiation transfer and the Earth's radiation balance. The temperature dependence of the molecular transmission function is calculated, and three steady states for Earth radiation balance are obtained. A type of the radiation balance, leading to "closing" of the atmospheric transmittance window 8-13 μm and development of the explosive greenhouse effect, is discussed.
Chursin A. A.
Falko M. V.
Golovko Vladimir F.
Gribanov Konstantin G.
Nikitin Alexei V.
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