Inverse problem of thermal sounding - Retrieval of the vertical profile of the absorption coefficient of the optically active component of a planetary atmosphere from observations of outgoing thermal radiation

Details Inverse problem of thermal sounding - Retrieval of the vertical profile of the absorption coefficient of the optically active component of a planetary atmosphere from observations of outgoing thermal radiation Inverse problem of thermal sounding - Retrieval of the vertical profile of the absorption coefficient of the optically active component of a planetary atmosphere from observations of outgoing thermal radiation

May 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990kosis..28..402u&link_type=abstract

Kosmicheskie Issledovaniia (ISSN 0023-4206), vol. 28, May-June 1990, p. 402-412. In Russian.

Computer Science

Sound

1

Absorptivity, Planetary Atmospheres, Thermal Radiation, Vertical Distribution, Aerosols, Atmospheric Sounding, Gas Mixtures, Integral Equations, Radiative Transfer, Spectrophotometry

Scientific paper

An expression for the kernal of the linearized inverse thermal-sounding problem for a planetary atmosphere is obtained by means of two methods: direct variations of the expression for the intensity of the outgoing thermal radiation and the use of solutions of the direct and conjugate problems of thermal radiation transfer. The results obtained can be used to retrieve the vertical profile of the extinction coefficient of purely absorbing aerosol and the gaseous-component mixture ratio.

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