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    Further Studies of a Lake Breeze Part ll: Theoretical Study

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 003::page 619
    Author:
    Estoque, Mariano A.
    ,
    Gross, James M.
    DOI: 10.1175/1520-0493(1981)109<0619:FSOALB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The three-dimensional structure and behavior of the lake-land breeze circulation which is induced by Lake Ontario is studied by means of a numerical model. The model is a primitive equation model which incorporates the effects of orography and the temperature prediction of the earth surface. A series of integrations is made in order to examine the effects of the large-scale prevailing flow and orography. These effects, which are found to be important in determining the structure of the lake-induced mesoscale flow pattern, are described in detail. One of the integrations corresponds to a simulation of an actually observed lake-land breeze circulation. Comparison between the simulated and the observed structures shows good agreement.
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      Further Studies of a Lake Breeze Part ll: Theoretical Study

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4200443
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    contributor authorEstoque, Mariano A.
    contributor authorGross, James M.
    date accessioned2017-06-09T16:03:19Z
    date available2017-06-09T16:03:19Z
    date copyright1981/03/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59841.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200443
    description abstractThe three-dimensional structure and behavior of the lake-land breeze circulation which is induced by Lake Ontario is studied by means of a numerical model. The model is a primitive equation model which incorporates the effects of orography and the temperature prediction of the earth surface. A series of integrations is made in order to examine the effects of the large-scale prevailing flow and orography. These effects, which are found to be important in determining the structure of the lake-induced mesoscale flow pattern, are described in detail. One of the integrations corresponds to a simulation of an actually observed lake-land breeze circulation. Comparison between the simulated and the observed structures shows good agreement.
    publisherAmerican Meteorological Society
    titleFurther Studies of a Lake Breeze Part ll: Theoretical Study
    typeJournal Paper
    journal volume109
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<0619:FSOALB>2.0.CO;2
    journal fristpage619
    journal lastpage634
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 003
    contenttypeFulltext
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