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    Estimation of Stratospheric Flow from Satellite 15-Micron Radiation

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 001::page 136
    Author:
    Zak, J. Allen
    ,
    Panofsky, H. A.
    DOI: 10.1175/1520-0450(1968)007<0136:EOSFFS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Ten-day average ?thermal winds? derived from TIROS VII in the CO2 band are compared to the corresponding geostrophic winds at 10 mb at latitudes 40?60N. The correlations for the west-east components are of order 0.8, those for the south-north components, 0.5. Much of the correlation in the U components is due to concurrent seasonal trend.
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      Estimation of Stratospheric Flow from Satellite 15-Micron Radiation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4218678
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    contributor authorZak, J. Allen
    contributor authorPanofsky, H. A.
    date accessioned2017-06-09T16:54:10Z
    date available2017-06-09T16:54:10Z
    date copyright1968/02/01
    date issued1968
    identifier issn0021-8952
    identifier otherams-7625.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218678
    description abstractTen-day average ?thermal winds? derived from TIROS VII in the CO2 band are compared to the corresponding geostrophic winds at 10 mb at latitudes 40?60N. The correlations for the west-east components are of order 0.8, those for the south-north components, 0.5. Much of the correlation in the U components is due to concurrent seasonal trend.
    publisherAmerican Meteorological Society
    titleEstimation of Stratospheric Flow from Satellite 15-Micron Radiation
    typeJournal Paper
    journal volume7
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1968)007<0136:EOSFFS>2.0.CO;2
    journal fristpage136
    journal lastpage140
    treeJournal of Applied Meteorology:;1968:;volume( 007 ):;issue: 001
    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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