On the thermodynamic evolution criteria with radiation effects of the global climate system

Details On the thermodynamic evolution criteria with radiation effects of the global climate system On the thermodynamic evolution criteria with radiation effects of the global climate system

Dec 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988angeo...6..645c&link_type=abstract

Annales Geophysicae (ISSN 0980-8752), vol. 6, Dec. 1988, p. 645-657.

Mathematics

Logic

7

Climate Change, Radiation Effects, Thermodynamics, Conductive Heat Transfer, Entropy, Radiation Absorption, Radiative Transfer

Scientific paper

The present consideration of integral entropy production theorems for the global earth-atmosphere system in terms of local irreversible thermodynamics establishes that, with the inclusion of radiant absorption and emission, global evolution criteria can be formulated with great generality and applied to typical meteorological-climatological conditions. Attention is given to the validity of the Glansdorff-Prigogine (1971) general evolution condition in the specific system considered, in which radiant phenomena and Fourier-type heat conduction are combined.

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