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    Convective Circulations Induced by Surface Heterogeneities

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 017::page 2915
    Author:
    Souza, Enio P.
    ,
    Rennó, Nilton O.
    ,
    Silva Dias, Maria A. F.
    DOI: 10.1175/1520-0469(2000)057<2915:CCIBSH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple theory for convective circulations induced by surface heterogeneities is proposed. The theory is based on the thermodynamics of heat engines and provides a simple physical explanation for the general characteristics of circulations forced by surface inhomogeneities in sloping terrains. In particular, the theory is applied to a mesoscale circulation induced by deforestation. It predicts that the intensity of the mesoscale convective circulation forced by deforestation depends on the difference of the near-surface nonadiabatic temperature and humidity between the forest and cleared regions and on the depth of the convective boundary layer. The theory was successfully tested against observations made during a field experiment in the Amazon forest and a nearby clearing.
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      Convective Circulations Induced by Surface Heterogeneities

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4159168
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    • Journal of the Atmospheric Sciences

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    contributor authorSouza, Enio P.
    contributor authorRennó, Nilton O.
    contributor authorSilva Dias, Maria A. F.
    date accessioned2017-06-09T14:36:29Z
    date available2017-06-09T14:36:29Z
    date copyright2000/09/01
    date issued2000
    identifier issn0022-4928
    identifier otherams-22690.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159168
    description abstractA simple theory for convective circulations induced by surface heterogeneities is proposed. The theory is based on the thermodynamics of heat engines and provides a simple physical explanation for the general characteristics of circulations forced by surface inhomogeneities in sloping terrains. In particular, the theory is applied to a mesoscale circulation induced by deforestation. It predicts that the intensity of the mesoscale convective circulation forced by deforestation depends on the difference of the near-surface nonadiabatic temperature and humidity between the forest and cleared regions and on the depth of the convective boundary layer. The theory was successfully tested against observations made during a field experiment in the Amazon forest and a nearby clearing.
    publisherAmerican Meteorological Society
    titleConvective Circulations Induced by Surface Heterogeneities
    typeJournal Paper
    journal volume57
    journal issue17
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2000)057<2915:CCIBSH>2.0.CO;2
    journal fristpage2915
    journal lastpage2922
    treeJournal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 017
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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