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    Boundary-Layer Growth over the Tropical Ocean

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 008::page 1762
    Author:
    Fitzjarrald, David R.
    ,
    Garstang, Michael
    DOI: 10.1175/1520-0493(1981)109<1762:BLGOTT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Results of a one-dimensional mixed-layer growth model are compared with thermodynamic observations made during the GARP Atlantic Tropical Experiment (GATE). Observed drying at low levels accompanying warming in the wake of a storm is hypothesized to be the result of rapid mixed-layer growth as well as of subsidence in the environment outside the storm. Sensitivity of the model solutions to changes in subsidence and stability above the mixed layer is shown. Model solutions show protracted recovery periods only when the wind speed near the surface is moderate (?3 m s?1). Recovery of the mixed layer in the wake of the 12 September 1974 GATE squall line is simulated by the model.
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      Boundary-Layer Growth over the Tropical Ocean

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4200549
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    contributor authorFitzjarrald, David R.
    contributor authorGarstang, Michael
    date accessioned2017-06-09T16:03:32Z
    date available2017-06-09T16:03:32Z
    date copyright1981/08/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59936.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200549
    description abstractResults of a one-dimensional mixed-layer growth model are compared with thermodynamic observations made during the GARP Atlantic Tropical Experiment (GATE). Observed drying at low levels accompanying warming in the wake of a storm is hypothesized to be the result of rapid mixed-layer growth as well as of subsidence in the environment outside the storm. Sensitivity of the model solutions to changes in subsidence and stability above the mixed layer is shown. Model solutions show protracted recovery periods only when the wind speed near the surface is moderate (?3 m s?1). Recovery of the mixed layer in the wake of the 12 September 1974 GATE squall line is simulated by the model.
    publisherAmerican Meteorological Society
    titleBoundary-Layer Growth over the Tropical Ocean
    typeJournal Paper
    journal volume109
    journal issue8
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<1762:BLGOTT>2.0.CO;2
    journal fristpage1762
    journal lastpage1772
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 008
    contenttypeFulltext
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