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    Implicit Differencing of Predictive Equations of the Boundary Layer

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 010::page 1321
    Author:
    Paegle, Jan
    ,
    Zdunkowski, Wilford G.
    ,
    Welch, Ronald M.
    DOI: 10.1175/1520-0493(1976)104<1321:IDOPEO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Crank-Nicholson method may not give useful results in detailed prediction of the thermal planetary boundary layer unless tune steps on the order of 10 s are used. In similar problems, lower order time differencing methods give reasonable results with time steps as large as 300 s. The reason for the superior behavior of the lower order schemes relative to straightforward application of the Crank-Nicholson technique is due to a better treatment of short waves which appear to be critically important in nonlinear terms.
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      Implicit Differencing of Predictive Equations of the Boundary Layer

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199524
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    • Monthly Weather Review

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    contributor authorPaegle, Jan
    contributor authorZdunkowski, Wilford G.
    contributor authorWelch, Ronald M.
    date accessioned2017-06-09T16:01:23Z
    date available2017-06-09T16:01:23Z
    date copyright1976/10/01
    date issued1976
    identifier issn0027-0644
    identifier otherams-59012.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199524
    description abstractThe Crank-Nicholson method may not give useful results in detailed prediction of the thermal planetary boundary layer unless tune steps on the order of 10 s are used. In similar problems, lower order time differencing methods give reasonable results with time steps as large as 300 s. The reason for the superior behavior of the lower order schemes relative to straightforward application of the Crank-Nicholson technique is due to a better treatment of short waves which appear to be critically important in nonlinear terms.
    publisherAmerican Meteorological Society
    titleImplicit Differencing of Predictive Equations of the Boundary Layer
    typeJournal Paper
    journal volume104
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1976)104<1321:IDOPEO>2.0.CO;2
    journal fristpage1321
    journal lastpage1324
    treeMonthly Weather Review:;1976:;volume( 104 ):;issue: 010
    contenttypeFulltext
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