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    A METHOD OF REPRESENTING THE HORIZONTAL PRESSURE FORCE WITHOUT REDUCTION OF STATION PRESSURES TO SEA LEVEL

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 002::page 166
    Author:
    Sangster, Wayne E.
    DOI: 10.1175/1520-0469(1960)017<0166:AMORTH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A coordinate system is presented in which the lowest coordinate surface represents the topography of the earth. Higher coordinate surfaces reflect this topography in diminishing degrees and become isobaric at and above the 500-mb level. A method of representing the field of the horizontal pressure force in the nonisobaric coordinate surfaces, using geostrophic stream and potential functions, is described. Geostrophic winds computed from these functions are compared with those obtained from the customary sea-level charts and with observed winds.
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      A METHOD OF REPRESENTING THE HORIZONTAL PRESSURE FORCE WITHOUT REDUCTION OF STATION PRESSURES TO SEA LEVEL

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150191
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    contributor authorSangster, Wayne E.
    date accessioned2017-06-09T14:12:19Z
    date available2017-06-09T14:12:19Z
    date copyright1960/04/01
    date issued1960
    identifier issn0095-9634
    identifier otherams-14610.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150191
    description abstractA coordinate system is presented in which the lowest coordinate surface represents the topography of the earth. Higher coordinate surfaces reflect this topography in diminishing degrees and become isobaric at and above the 500-mb level. A method of representing the field of the horizontal pressure force in the nonisobaric coordinate surfaces, using geostrophic stream and potential functions, is described. Geostrophic winds computed from these functions are compared with those obtained from the customary sea-level charts and with observed winds.
    publisherAmerican Meteorological Society
    titleA METHOD OF REPRESENTING THE HORIZONTAL PRESSURE FORCE WITHOUT REDUCTION OF STATION PRESSURES TO SEA LEVEL
    typeJournal Paper
    journal volume17
    journal issue2
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1960)017<0166:AMORTH>2.0.CO;2
    journal fristpage166
    journal lastpage176
    treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 002
    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
    yabeshDSpacePersian