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    A Time-Dependent Lateral Boundary Scheme for Limited-Area Primitive Equation Models

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 006::page 744
    Author:
    Perkey, Donald J.
    ,
    Kreitzberg, Carl W.
    DOI: 10.1175/1520-0493(1976)104<0744:ATDLBS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Before high-resolution numerical models can be of use operationally, they must be restricted to a limited domain, thus necessitating lateral boundary conditions which allow the changes outside the limited domain to influence the results while not contaminating the forecast with spurious boundary-reflected energy. Such a set of time-dependent lateral boundary conditions are presented in this paper. This boundary condition set is investigated using the linear analytic and finite-difference advection equations, the non-linear finite-difference shallow-water equations, and the hydrostatic primitive equations. The results illustrate how the boundary condition transforms long- and medium-length interior advective and gravity waves into short waves which can then be removed by a low pass filter, thereby giving the appearance that the exiting wave simply passed through the boundary. The results also indicate that large-scale advective and gravity waves enter the forecast domain with little degradation. Thus, from the tests performed, the described boundary condition scheme yields a practical solution for prescribing time-dependent lateral boundaries for a limited-area model.
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      A Time-Dependent Lateral Boundary Scheme for Limited-Area Primitive Equation Models

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199435
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    • Monthly Weather Review

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    contributor authorPerkey, Donald J.
    contributor authorKreitzberg, Carl W.
    date accessioned2017-06-09T16:01:12Z
    date available2017-06-09T16:01:12Z
    date copyright1976/06/01
    date issued1976
    identifier issn0027-0644
    identifier otherams-58933.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199435
    description abstractBefore high-resolution numerical models can be of use operationally, they must be restricted to a limited domain, thus necessitating lateral boundary conditions which allow the changes outside the limited domain to influence the results while not contaminating the forecast with spurious boundary-reflected energy. Such a set of time-dependent lateral boundary conditions are presented in this paper. This boundary condition set is investigated using the linear analytic and finite-difference advection equations, the non-linear finite-difference shallow-water equations, and the hydrostatic primitive equations. The results illustrate how the boundary condition transforms long- and medium-length interior advective and gravity waves into short waves which can then be removed by a low pass filter, thereby giving the appearance that the exiting wave simply passed through the boundary. The results also indicate that large-scale advective and gravity waves enter the forecast domain with little degradation. Thus, from the tests performed, the described boundary condition scheme yields a practical solution for prescribing time-dependent lateral boundaries for a limited-area model.
    publisherAmerican Meteorological Society
    titleA Time-Dependent Lateral Boundary Scheme for Limited-Area Primitive Equation Models
    typeJournal Paper
    journal volume104
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1976)104<0744:ATDLBS>2.0.CO;2
    journal fristpage744
    journal lastpage755
    treeMonthly Weather Review:;1976:;volume( 104 ):;issue: 006
    contenttypeFulltext
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