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    Estimating the Depth of the Daytime Convective Boundary Layer

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 008::page 1123
    Author:
    Kaimal, J. C.
    ,
    Abshire, N. L.
    ,
    Chadwick, R. B.
    ,
    Decker, M. T.
    ,
    Hooke, W. H.
    ,
    Kropfli, R. A.
    ,
    Neff, W. D.
    ,
    Pasqualucci, F.
    ,
    Hildebrand, P. H.
    DOI: 10.1175/1520-0450(1982)021<1123:ETDOTD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Three in-situ and five remote sensing techniques for measuring the height of the daytime convective boundary layer were compared. There was, as a rule, good agreement between the different systems when the capping inversion was steep and well defined, and some variability when the stratification was not so sharply defined. Two indirect methods for estimating boundary-layer heights from the length scales of convective motions in the layer are also discussed.
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      Estimating the Depth of the Daytime Convective Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145422
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    • Journal of Applied Meteorology

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    contributor authorKaimal, J. C.
    contributor authorAbshire, N. L.
    contributor authorChadwick, R. B.
    contributor authorDecker, M. T.
    contributor authorHooke, W. H.
    contributor authorKropfli, R. A.
    contributor authorNeff, W. D.
    contributor authorPasqualucci, F.
    contributor authorHildebrand, P. H.
    date accessioned2017-06-09T13:58:56Z
    date available2017-06-09T13:58:56Z
    date copyright1982/08/01
    date issued1982
    identifier issn0021-8952
    identifier otherams-10318.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145422
    description abstractThree in-situ and five remote sensing techniques for measuring the height of the daytime convective boundary layer were compared. There was, as a rule, good agreement between the different systems when the capping inversion was steep and well defined, and some variability when the stratification was not so sharply defined. Two indirect methods for estimating boundary-layer heights from the length scales of convective motions in the layer are also discussed.
    publisherAmerican Meteorological Society
    titleEstimating the Depth of the Daytime Convective Boundary Layer
    typeJournal Paper
    journal volume21
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1982)021<1123:ETDOTD>2.0.CO;2
    journal fristpage1123
    journal lastpage1129
    treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 008
    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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