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    Boundary-Layer Damping of Baroclinic Instability

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 005::page 772
    Author:
    Staley, D. O.
    DOI: 10.1175/1520-0469(1993)050<0772:BLDOBI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A shooting method is applied to a 100-level perturbation model with an explicit Ekman layer. Growth rates for a no-slip boundary condition are similar to those found previously. It is noted that the large cross-isobaric flow of the classic Ekman solution overestimates the damping by roughly a factor of 2. For the condition of zero vertical gradient of perturbation streamfunction at the lower boundary (allowing slip), growth rates are only slightly reduced from the frictionless case. The physical bases for an implicit boundary layer, as well as the no-slip condition, are questioned.
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      Boundary-Layer Damping of Baroclinic Instability

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    contributor authorStaley, D. O.
    date accessioned2017-06-09T14:31:19Z
    date available2017-06-09T14:31:19Z
    date copyright1993/03/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20868.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157143
    description abstractA shooting method is applied to a 100-level perturbation model with an explicit Ekman layer. Growth rates for a no-slip boundary condition are similar to those found previously. It is noted that the large cross-isobaric flow of the classic Ekman solution overestimates the damping by roughly a factor of 2. For the condition of zero vertical gradient of perturbation streamfunction at the lower boundary (allowing slip), growth rates are only slightly reduced from the frictionless case. The physical bases for an implicit boundary layer, as well as the no-slip condition, are questioned.
    publisherAmerican Meteorological Society
    titleBoundary-Layer Damping of Baroclinic Instability
    typeJournal Paper
    journal volume50
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<0772:BLDOBI>2.0.CO;2
    journal fristpage772
    journal lastpage777
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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