Rosseland coefficients of optically dense atmospheres consisting of CO2 and H2O

Details Rosseland coefficients of optically dense atmospheres consisting of CO2 and H2O Rosseland coefficients of optically dense atmospheres consisting of CO2 and H2O

May 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980kosis..18..464g&link_type=abstract

Kosmicheskie Issledovaniia, vol. 18, May-June 1980, p. 464-466. In Russian.

Physics

Optics

1

Atmospheric Optics, Carbon Dioxide, Heat Transfer, Planetary Atmospheres, Water Vapor, Atmospheric Density, Atmospheric Pressure, Atmospheric Temperature, Optical Density

Scientific paper

Rosseland coefficients are calculated for atmospheres consisting of carbon dioxide and water vapor. In relation to the absorption coefficient and the Planck function, the Rosseland coefficients are shown to be dependent on temperature and pressure. Therefore Rosseland coefficients have been computed for a wide range of parameters: temperatures of 300-2000 K, pressures of 0.5-100 atm, and varying concentrations of CO2 and H2O.

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