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    PREDICTIVE CONSEQUENCES OF CERTAIN PHYSICAL INCONSISTENCIES IN THE GEOSTROPHIC BAROTROPIC MODEL

    Source: Monthly Weather Review:;1957:;volume( 085 ):;issue: 007::page 229
    Author:
    SHUMAN, FREDERICK G.
    DOI: 10.1175/1520-0493(1957)085<0229:PCOCPI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The physical inconsistency of geostrophic flow and small surface pressure tendencies is discussed. The frequently disastrous consequences in conventional geostrophic barotropic predictions are numerically identified by comparisons with experimental ?semi-geostrophic? barotropic predictions from which the inconsistency has been removed. Effects of the inconsistency of the geostrophic wind field with the equations of motion are also quantitatively isolated by comparisons of semi-geostrophic predictions with predictions made with wind fields which satisfy the balance equation. It is concluded that the principal fault of the conventional geostrophic approximation lies in the violation of the continuity equation. Its lack of the dynamic effects expressed in the equations of motion seems also significant, but is less important.
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      PREDICTIVE CONSEQUENCES OF CERTAIN PHYSICAL INCONSISTENCIES IN THE GEOSTROPHIC BAROTROPIC MODEL

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4197217
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    contributor authorSHUMAN, FREDERICK G.
    date accessioned2017-06-09T15:55:59Z
    date available2017-06-09T15:55:59Z
    date copyright1957/07/01
    date issued1957
    identifier issn0027-0644
    identifier otherams-56937.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197217
    description abstractThe physical inconsistency of geostrophic flow and small surface pressure tendencies is discussed. The frequently disastrous consequences in conventional geostrophic barotropic predictions are numerically identified by comparisons with experimental ?semi-geostrophic? barotropic predictions from which the inconsistency has been removed. Effects of the inconsistency of the geostrophic wind field with the equations of motion are also quantitatively isolated by comparisons of semi-geostrophic predictions with predictions made with wind fields which satisfy the balance equation. It is concluded that the principal fault of the conventional geostrophic approximation lies in the violation of the continuity equation. Its lack of the dynamic effects expressed in the equations of motion seems also significant, but is less important.
    publisherAmerican Meteorological Society
    titlePREDICTIVE CONSEQUENCES OF CERTAIN PHYSICAL INCONSISTENCIES IN THE GEOSTROPHIC BAROTROPIC MODEL
    typeJournal Paper
    journal volume85
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1957)085<0229:PCOCPI>2.0.CO;2
    journal fristpage229
    journal lastpage234
    treeMonthly Weather Review:;1957:;volume( 085 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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