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    Algorithms for Obtaining Atmospheric Surface-Layer Fluxes from Scintillation Measurements

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 003::page 456
    Author:
    Hill, Reginald J.
    DOI: 10.1175/1520-0426(1997)014<0456:AFOASL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Algorithms are derived for obtaining atmospheric surface-layer fluxes of heat, humidity, and momentum from scintillation measurements. Both the three-wavelength and two-wavelength methods are examined, as is combining the two-wavelength method with other micrometeorological measurements. Corrections for the effects of strong scintillation are discussed. Deriving turbulence inner-scale and refractive structure parameters from scintillation variances is discussed, as is using these quantities to obtain the energy dissipation rate and structure parameters of temperature and humidity. Given these latter quantities, Monin?Obukhov similarity theory is applied to specific humidity and temperature (equivalently, potential temperature) to obtain the fluxes.
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      Algorithms for Obtaining Atmospheric Surface-Layer Fluxes from Scintillation Measurements

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147957
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    contributor authorHill, Reginald J.
    date accessioned2017-06-09T14:06:35Z
    date available2017-06-09T14:06:35Z
    date copyright1997/06/01
    date issued1997
    identifier issn0739-0572
    identifier otherams-1260.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147957
    description abstractAlgorithms are derived for obtaining atmospheric surface-layer fluxes of heat, humidity, and momentum from scintillation measurements. Both the three-wavelength and two-wavelength methods are examined, as is combining the two-wavelength method with other micrometeorological measurements. Corrections for the effects of strong scintillation are discussed. Deriving turbulence inner-scale and refractive structure parameters from scintillation variances is discussed, as is using these quantities to obtain the energy dissipation rate and structure parameters of temperature and humidity. Given these latter quantities, Monin?Obukhov similarity theory is applied to specific humidity and temperature (equivalently, potential temperature) to obtain the fluxes.
    publisherAmerican Meteorological Society
    titleAlgorithms for Obtaining Atmospheric Surface-Layer Fluxes from Scintillation Measurements
    typeJournal Paper
    journal volume14
    journal issue3
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1997)014<0456:AFOASL>2.0.CO;2
    journal fristpage456
    journal lastpage467
    treeJournal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 003
    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