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    A Nonreflecting Upper Boundary Condition for Anelastic Nonhydrostatic Mesoscale Gravity-Wave Models

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 004::page 1249
    Author:
    Kim, Young-Joon
    ,
    Kar, Sajal K.
    ,
    Arakawa, Akio
    DOI: 10.1175/1520-0493(1993)121<1249:ANUBCF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A sponge layer is formulated to prevent spurious reflection of vertically propagating quasi-stationary gravity waves at the upper boundary of a two-dimensional numerical anelastic nonhydrostatic model. The sponge layer includes damping of both Newtonian-cooling type and Rayleigh-friction type, whose coefficients are determined in such a way that the reflectivity of wave energy at the bottom of the layer is zero. Unlike the formulations in earlier studies, our formulation includes the effects of vertical discretization, vertical mean density variation, and nonhydrostaticity. This sponge formulation is found effective in suppressing false downward reflection of waves for various types of quasi-stationary forcing.
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      A Nonreflecting Upper Boundary Condition for Anelastic Nonhydrostatic Mesoscale Gravity-Wave Models

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203040
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    contributor authorKim, Young-Joon
    contributor authorKar, Sajal K.
    contributor authorArakawa, Akio
    date accessioned2017-06-09T16:09:20Z
    date available2017-06-09T16:09:20Z
    date copyright1993/04/01
    date issued1993
    identifier issn0027-0644
    identifier otherams-62177.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203040
    description abstractA sponge layer is formulated to prevent spurious reflection of vertically propagating quasi-stationary gravity waves at the upper boundary of a two-dimensional numerical anelastic nonhydrostatic model. The sponge layer includes damping of both Newtonian-cooling type and Rayleigh-friction type, whose coefficients are determined in such a way that the reflectivity of wave energy at the bottom of the layer is zero. Unlike the formulations in earlier studies, our formulation includes the effects of vertical discretization, vertical mean density variation, and nonhydrostaticity. This sponge formulation is found effective in suppressing false downward reflection of waves for various types of quasi-stationary forcing.
    publisherAmerican Meteorological Society
    titleA Nonreflecting Upper Boundary Condition for Anelastic Nonhydrostatic Mesoscale Gravity-Wave Models
    typeJournal Paper
    journal volume121
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1993)121<1249:ANUBCF>2.0.CO;2
    journal fristpage1249
    journal lastpage1261
    treeMonthly Weather Review:;1993:;volume( 121 ):;issue: 004
    contenttypeFulltext
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