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    Stratified Flow over Two-Dimensional Topography in Fluid of Infinite Depth: A Laboratory Simulation

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 015::page 1614
    Author:
    Baines, Peter G.
    ,
    Hoinka, Klaus P.
    DOI: 10.1175/1520-0469(1985)042<1614:SFOTDT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper describes some laboratory experiments with two-dimensional stratified flow over isolated topography, in which a novel configuration simulating a radiating upper boundary condition is employed. Several experimental tests show that the upper boundary is quite effective in absorbing energy. The properties of flow over five different obstacle shapes were obtained for a merge of values of the parameter Nh/U(h is obstacle height, N Brunt-Väisälä frequency and U towing velocity) from 0 to 4 (approximately). The main results of the study are 1) for 0 ≤ Nh/U ≤ 0.5 (±0.2), the flow is consistent with linear theory and Longs model; 2) for 0.5 ? Nh/U ? 2.0, upstream columnar disturbances are found which apparently propagate arbitrarily far upstream in an inviscid system. 3) overturning and rotors in the lee wave field occur for Nh/U ? 1.5; and 4) for Nh/U ? 2.0, blocked fluid is present upstream, and in some cases is also apparent downstream. This upstream blocking is due to the super-position of the propagating columnar disturbances; it will similarly extend arbitrarily far upstream given sufficient time.
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      Stratified Flow over Two-Dimensional Topography in Fluid of Infinite Depth: A Laboratory Simulation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155180
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    contributor authorBaines, Peter G.
    contributor authorHoinka, Klaus P.
    date accessioned2017-06-09T14:25:48Z
    date available2017-06-09T14:25:48Z
    date copyright1985/08/01
    date issued1985
    identifier issn0022-4928
    identifier otherams-19100.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155180
    description abstractThis paper describes some laboratory experiments with two-dimensional stratified flow over isolated topography, in which a novel configuration simulating a radiating upper boundary condition is employed. Several experimental tests show that the upper boundary is quite effective in absorbing energy. The properties of flow over five different obstacle shapes were obtained for a merge of values of the parameter Nh/U(h is obstacle height, N Brunt-Väisälä frequency and U towing velocity) from 0 to 4 (approximately). The main results of the study are 1) for 0 ≤ Nh/U ≤ 0.5 (±0.2), the flow is consistent with linear theory and Longs model; 2) for 0.5 ? Nh/U ? 2.0, upstream columnar disturbances are found which apparently propagate arbitrarily far upstream in an inviscid system. 3) overturning and rotors in the lee wave field occur for Nh/U ? 1.5; and 4) for Nh/U ? 2.0, blocked fluid is present upstream, and in some cases is also apparent downstream. This upstream blocking is due to the super-position of the propagating columnar disturbances; it will similarly extend arbitrarily far upstream given sufficient time.
    publisherAmerican Meteorological Society
    titleStratified Flow over Two-Dimensional Topography in Fluid of Infinite Depth: A Laboratory Simulation
    typeJournal Paper
    journal volume42
    journal issue15
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1985)042<1614:SFOTDT>2.0.CO;2
    journal fristpage1614
    journal lastpage1630
    treeJournal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 015
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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