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Laboratory measurement of the temperature dependence of gaseous sulfur dioxide (SO 2 ) microwave absorption with application to the Venus atmosphere
Author(s) -
Suleiman Shady H.,
Kolodner Marc A.,
Steffes Paul G.
Publication year - 1996
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/95je03728
Subject(s) - atmosphere of venus , venus , microwave , opacity , atmosphere (unit) , radiative transfer , sulfur dioxide , molar absorptivity , materials science , atmospheric radiative transfer codes , absorption spectroscopy , computational physics , analytical chemistry (journal) , physics , optics , chemistry , astrobiology , meteorology , inorganic chemistry , chromatography , quantum mechanics
High‐accuracy laboratory measurements of the temperature dependence of the opacity from gaseous sulfur dioxide (SO 2 ) in a carbon dioxide (CO 2 ) atmosphere at temperatures from 290 to 505 K and at pressures from 1 to 4 atm have been conducted at frequencies of 2.25 GHz (13.3 cm), 8.5 GHz (3.5 cm), and 21.7 GHz (1.4 cm). Based on these absorptivity measurements, a Ben‐Reuven (BR) line shape model has been developed that provides a more accurate characterization of the microwave absorption of gaseous SO 2 in the Venus atmosphere as compared with other formalisms. The developed BR formalism is incorporated into a radiative transfer model. The resulting microwave emission spectrum of Venus is then used to set an upper limit on the disk‐averaged abundance of gaseous SO 2 below the main cloud layer. It is found that gaseous SO 2 has an upper limit of 150 ppm, which compares well with previous spacecraft in situ measurements and Earth‐based radio astronomical observations.

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