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    Effect of Cloud Scattering on Line Formation in the Atmosphere of Venus

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003::page 511
    Author:
    Potter, J. F.
    DOI: 10.1175/1520-0469(1969)026<0511:EOCSOL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Corrections for anisotropic scattering in a cloudy medium are added to a synthetic spectrum analysis by Belton, Hunten and Goody of CO2 bands and a water vapor line in the spectrum of Venus. It is found that to a good approximation the introduction of anisotropic scattering merely renormalizes the theoretical curves so that the corrections can be applied without recalculating the synthetic spectra. Since the line shapes and relative intensities are unaltered, derived pressures and temperatures remain the same. The corrected results indicate that the scattering mean free path in the Cytherian clouds resembles that for terrestrial cirrus clouds and that there is at least 20 times too little water vapor present to be in equilibrium with a water or ice cloud.
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      Effect of Cloud Scattering on Line Formation in the Atmosphere of Venus

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151300
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    contributor authorPotter, J. F.
    date accessioned2017-06-09T14:14:52Z
    date available2017-06-09T14:14:52Z
    date copyright1969/05/01
    date issued1969
    identifier issn0022-4928
    identifier otherams-15609.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151300
    description abstractCorrections for anisotropic scattering in a cloudy medium are added to a synthetic spectrum analysis by Belton, Hunten and Goody of CO2 bands and a water vapor line in the spectrum of Venus. It is found that to a good approximation the introduction of anisotropic scattering merely renormalizes the theoretical curves so that the corrections can be applied without recalculating the synthetic spectra. Since the line shapes and relative intensities are unaltered, derived pressures and temperatures remain the same. The corrected results indicate that the scattering mean free path in the Cytherian clouds resembles that for terrestrial cirrus clouds and that there is at least 20 times too little water vapor present to be in equilibrium with a water or ice cloud.
    publisherAmerican Meteorological Society
    titleEffect of Cloud Scattering on Line Formation in the Atmosphere of Venus
    typeJournal Paper
    journal volume26
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1969)026<0511:EOCSOL>2.0.CO;2
    journal fristpage511
    journal lastpage517
    treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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