YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    NOTES AND CORRESPONDECEScaling Reasoning and Field Data on the Sea Surface Roughness Lengths for Scalars

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 003::page 320
    Author:
    Zilitinkevich, S. S.
    ,
    Grachev, A. A.
    ,
    Fairall, C. W.
    DOI: 10.1175/1520-0469(2001)058<0320:NACRAF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The heat and mass transfer over the sea is considered in terms of the sea surface roughness lengths for scalars, z0T for potential temperature ?, and z0q for specific humidity q, or alternatively, in terms of the roughness-layer scalar increments, δ? and δq. A new scaling reasoning is proposed in support of the familiar square root dependence of the above increments on the roughness Reynolds number, Re0u = z0uu?/?, where z0u is the sea surface aerodynamic roughness length, u? is the friction velocity, and ? is the molecular viscosity of the air. Scaling predictions are validated using data from measurements made by the National Oceanic and Atmospheric Administration?s Environmental Technology Laboratory aboard the R/V Moana Wave in the Tropical Ocean Global Atmosphere Coupled Ocean?Atmosphere Response Experiment in 1992?93 and the R/P FLIP in the San Clemente Ocean Probing Experiment in September 1993. Data presented as the dimensionless scalar increments (or the ratios z0u/z0T and z0u/z0q) versus Re0u show a good agreement with theoretical predictions, especially at Re0u > 2 (over stormy sea). The resulting roughness-length formulations are recommended for practical use in climate and mesoscale air?sea interaction models.
    • Download: (116.8Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      NOTES AND CORRESPONDECEScaling Reasoning and Field Data on the Sea Surface Roughness Lengths for Scalars

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4159261
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorZilitinkevich, S. S.
    contributor authorGrachev, A. A.
    contributor authorFairall, C. W.
    date accessioned2017-06-09T14:36:41Z
    date available2017-06-09T14:36:41Z
    date copyright2001/02/01
    date issued2001
    identifier issn0022-4928
    identifier otherams-22774.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159261
    description abstractThe heat and mass transfer over the sea is considered in terms of the sea surface roughness lengths for scalars, z0T for potential temperature ?, and z0q for specific humidity q, or alternatively, in terms of the roughness-layer scalar increments, δ? and δq. A new scaling reasoning is proposed in support of the familiar square root dependence of the above increments on the roughness Reynolds number, Re0u = z0uu?/?, where z0u is the sea surface aerodynamic roughness length, u? is the friction velocity, and ? is the molecular viscosity of the air. Scaling predictions are validated using data from measurements made by the National Oceanic and Atmospheric Administration?s Environmental Technology Laboratory aboard the R/V Moana Wave in the Tropical Ocean Global Atmosphere Coupled Ocean?Atmosphere Response Experiment in 1992?93 and the R/P FLIP in the San Clemente Ocean Probing Experiment in September 1993. Data presented as the dimensionless scalar increments (or the ratios z0u/z0T and z0u/z0q) versus Re0u show a good agreement with theoretical predictions, especially at Re0u > 2 (over stormy sea). The resulting roughness-length formulations are recommended for practical use in climate and mesoscale air?sea interaction models.
    publisherAmerican Meteorological Society
    titleNOTES AND CORRESPONDECEScaling Reasoning and Field Data on the Sea Surface Roughness Lengths for Scalars
    typeJournal Paper
    journal volume58
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2001)058<0320:NACRAF>2.0.CO;2
    journal fristpage320
    journal lastpage325
    treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 003
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian