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    Interpretation of the Mariner 5 Lyman Alpha Measurements

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 004::page 564
    Author:
    Barth, Charles A.
    DOI: 10.1175/1520-0469(1968)025<0564:IOTMLA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Mariner 5 Lyman alpha measurements can be fitted with the barometric-exospheric equation only if a two-component model atmosphere is used. Of the three possible hypotheses to explain such an atmosphere, the model containing a mixture of atomic hydrogen and molecular hydrogen is preferred over the atomic hydrogen-deuterium model or the atomic hydrogen two-temperature model. The source of molecular hydrogen in the upper atmosphere may be chemical reactions either in the hot, dense lower atmosphere or in the upper atmosphere. The photodissociation of molecular hydrogen produces atoms with excess kinetic energy which either escape from the planetary gravitational field or react with the molecules in the lower atmosphere. The presence of molecular hydrogen affects calculations of the temperature of the Venus upper atmosphere as well as its ionic and chemical structure.
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      Interpretation of the Mariner 5 Lyman Alpha Measurements

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4151132
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    contributor authorBarth, Charles A.
    date accessioned2017-06-09T14:14:29Z
    date available2017-06-09T14:14:29Z
    date copyright1968/07/01
    date issued1968
    identifier issn0022-4928
    identifier otherams-15458.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151132
    description abstractThe Mariner 5 Lyman alpha measurements can be fitted with the barometric-exospheric equation only if a two-component model atmosphere is used. Of the three possible hypotheses to explain such an atmosphere, the model containing a mixture of atomic hydrogen and molecular hydrogen is preferred over the atomic hydrogen-deuterium model or the atomic hydrogen two-temperature model. The source of molecular hydrogen in the upper atmosphere may be chemical reactions either in the hot, dense lower atmosphere or in the upper atmosphere. The photodissociation of molecular hydrogen produces atoms with excess kinetic energy which either escape from the planetary gravitational field or react with the molecules in the lower atmosphere. The presence of molecular hydrogen affects calculations of the temperature of the Venus upper atmosphere as well as its ionic and chemical structure.
    publisherAmerican Meteorological Society
    titleInterpretation of the Mariner 5 Lyman Alpha Measurements
    typeJournal Paper
    journal volume25
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1968)025<0564:IOTMLA>2.0.CO;2
    journal fristpage564
    journal lastpage567
    treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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