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    A Linear Model of Boundary Layer Flow Applied to the St. Patrick's Day Storm of 1965

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 007::page 1151
    Author:
    Naistat, Richard J.
    ,
    Young, John A.
    DOI: 10.1175/1520-0450(1973)012<1151:ALMOBL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A time-dependent, one-dimensional numerical model of the boundary layer at individual stations is solved by a finite-difference technique for the St. Patrick's Day storm of 1965. Using only surface pressure and temperature gradients at 3-hr intervals as input, the model predicts the changing boundary layer wind profile at each of 225 grid points covering the central and eastern United States. Predicted winds are used to evaluate horizontal flow structure, vertical motion, three-dimensional trajectories, and flow acceleration. Modeled fields are compared to those corresponding to simple steady-state solutions and to observed data. The solution of the equations of motion retains the local acceleration and baroclinity, omits the nonlinear advection terms, and contains a damping effect in order to control the inertial-like oscillations which have complicated previous models. With the damping included, the model reasonably predicts the location of the low-level jet core, the vertical motion distribution, and, qualitatively, the orientation of the local acceleration in the boundary layer. The model-forecast ascent is well correlated with the observed precipitation rate when adequate surface moisture is available.
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      A Linear Model of Boundary Layer Flow Applied to the St. Patrick's Day Storm of 1965

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4229989
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    • Journal of Applied Meteorology

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    contributor authorNaistat, Richard J.
    contributor authorYoung, John A.
    date accessioned2017-06-09T17:30:27Z
    date available2017-06-09T17:30:27Z
    date copyright1973/10/01
    date issued1973
    identifier issn0021-8952
    identifier otherams-8643.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229989
    description abstractA time-dependent, one-dimensional numerical model of the boundary layer at individual stations is solved by a finite-difference technique for the St. Patrick's Day storm of 1965. Using only surface pressure and temperature gradients at 3-hr intervals as input, the model predicts the changing boundary layer wind profile at each of 225 grid points covering the central and eastern United States. Predicted winds are used to evaluate horizontal flow structure, vertical motion, three-dimensional trajectories, and flow acceleration. Modeled fields are compared to those corresponding to simple steady-state solutions and to observed data. The solution of the equations of motion retains the local acceleration and baroclinity, omits the nonlinear advection terms, and contains a damping effect in order to control the inertial-like oscillations which have complicated previous models. With the damping included, the model reasonably predicts the location of the low-level jet core, the vertical motion distribution, and, qualitatively, the orientation of the local acceleration in the boundary layer. The model-forecast ascent is well correlated with the observed precipitation rate when adequate surface moisture is available.
    publisherAmerican Meteorological Society
    titleA Linear Model of Boundary Layer Flow Applied to the St. Patrick's Day Storm of 1965
    typeJournal Paper
    journal volume12
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1973)012<1151:ALMOBL>2.0.CO;2
    journal fristpage1151
    journal lastpage1162
    treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 007
    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