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    Determining the Power-Law Wind-Profile Exponent under Near-Neutral Stability Conditions at Sea

    Source: Journal of Applied Meteorology:;1994:;volume( 033 ):;issue: 006::page 757
    Author:
    Hsu, S. A.
    ,
    Meindl, Eric A.
    ,
    Gilhousen, David B.
    DOI: 10.1175/1520-0450(1994)033<0757:DTPLWP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: On the basis of 30 samples from near-simultaneous overwater measurements by pairs of anemometers located at different heights in the Gulf of Mexico and off the Chesapeake Bay, Virginia, the mean and standard deviation for the exponent of the power-law wind profile over the ocean under near-neutral atmospheric stability conditions were determined to be 0.11 ± 0.03. Because this mean value is obtained from both deep and shallow water environments, it is recommended for use at sea to adjust the wind speed measurements at different heights to the standard height of 10 m above the mean sea surface. An example to apply this P value to estimate the momentum flux or wind stress is provided.
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      Determining the Power-Law Wind-Profile Exponent under Near-Neutral Stability Conditions at Sea

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147348
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    contributor authorHsu, S. A.
    contributor authorMeindl, Eric A.
    contributor authorGilhousen, David B.
    date accessioned2017-06-09T14:04:54Z
    date available2017-06-09T14:04:54Z
    date copyright1994/06/01
    date issued1994
    identifier issn0894-8763
    identifier otherams-12051.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147348
    description abstractOn the basis of 30 samples from near-simultaneous overwater measurements by pairs of anemometers located at different heights in the Gulf of Mexico and off the Chesapeake Bay, Virginia, the mean and standard deviation for the exponent of the power-law wind profile over the ocean under near-neutral atmospheric stability conditions were determined to be 0.11 ± 0.03. Because this mean value is obtained from both deep and shallow water environments, it is recommended for use at sea to adjust the wind speed measurements at different heights to the standard height of 10 m above the mean sea surface. An example to apply this P value to estimate the momentum flux or wind stress is provided.
    publisherAmerican Meteorological Society
    titleDetermining the Power-Law Wind-Profile Exponent under Near-Neutral Stability Conditions at Sea
    typeJournal Paper
    journal volume33
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1994)033<0757:DTPLWP>2.0.CO;2
    journal fristpage757
    journal lastpage765
    treeJournal of Applied Meteorology:;1994:;volume( 033 ):;issue: 006
    contenttypeFulltext
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