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    The Extrapolation of Vertical Profiles of Wind Speed within the Marine Atmospheric Surface layer Using the p Formula

    Source: Journal of Applied Meteorology:;1988:;volume( 027 ):;issue: 002::page 174
    Author:
    Segal, M.
    ,
    Pielke, R. A.
    DOI: 10.1175/1520-0450(1988)027<0174:TEOVPO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Values of p for the exponent-type wind profile formulation, used in vertical extrapolations of wind speed, were derived for the marine atmospheric surface layer. Nomograms were constructed providing p values as dependent on a single elevation measurement of the air temperature, wind speed, and the surface water temperature. The range of p values in the unstable surface layer is between 0.02 to 0.2, while for stable situations the range is 0.1 to possibly ?1.0. The values of p converge to about 0.2 for high wind speeds.
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      The Extrapolation of Vertical Profiles of Wind Speed within the Marine Atmospheric Surface layer Using the p Formula

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146509
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    contributor authorSegal, M.
    contributor authorPielke, R. A.
    date accessioned2017-06-09T14:02:11Z
    date available2017-06-09T14:02:11Z
    date copyright1988/02/01
    date issued1988
    identifier issn0894-8763
    identifier otherams-11297.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146509
    description abstractValues of p for the exponent-type wind profile formulation, used in vertical extrapolations of wind speed, were derived for the marine atmospheric surface layer. Nomograms were constructed providing p values as dependent on a single elevation measurement of the air temperature, wind speed, and the surface water temperature. The range of p values in the unstable surface layer is between 0.02 to 0.2, while for stable situations the range is 0.1 to possibly ?1.0. The values of p converge to about 0.2 for high wind speeds.
    publisherAmerican Meteorological Society
    titleThe Extrapolation of Vertical Profiles of Wind Speed within the Marine Atmospheric Surface layer Using the p Formula
    typeJournal Paper
    journal volume27
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1988)027<0174:TEOVPO>2.0.CO;2
    journal fristpage174
    journal lastpage181
    treeJournal of Applied Meteorology:;1988:;volume( 027 ):;issue: 002
    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
    yabeshDSpacePersian