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    Observational Study of Marine Atmospheric Boundary Layer Characteristics during Swell

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009::page 2747
    Author:
    Smedman, A.
    ,
    Högström, U.
    ,
    Sahleé, E.
    ,
    Drennan, W. M.
    ,
    Kahma, K. K.
    ,
    Pettersson, H.
    ,
    Zhang, F.
    DOI: 10.1175/2009JAS2952.1
    Publisher: American Meteorological Society
    Abstract: By combining simultaneous data from an instrumented Air?Sea Interaction Spar (ASIS) buoy and a 30-m tower, profiles of wind and turbulence characteristics have been obtained at several heights from about 1 to 30 m above the water surface during swell conditions. Five cases formed as averages over time periods ranging from 2.5 to 9.5 h, representing quasi-steady conditions, have been selected. They represent a range of typical wave age and include wind-following swell cases and cross-swell cases. For relatively large wave age, the wind profile exhibits a well-defined maximum in the height range 5?10 m; for more modest wave age, this maximum turns into a sharp ?knee? in the wind profile. Below the maximum (or knee), the wind increases rapidly with height; above that point the wind is very nearly constant up to the highest measuring level on the tower, 30 m. Analysis of balloon data from one day with swell indicates that the layer with constant wind in fact extends to the top of the boundary layer, in this case ?200 m. Analysis of the complete swell dataset from the 45 days of the 2003 Baltic Swell experiment shows that the results concerning wind profile shape obtained from the selected cases are generally valid in this experiment. Analysis of the nondimensional wind profile ?m shows that Monin?Obukhov scaling is not valid during swell. Wind and turbulence characteristics are found not to vary to a significant degree with the wind/swell angle within the range of angles encountered, ±90°.
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      Observational Study of Marine Atmospheric Boundary Layer Characteristics during Swell

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209976
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    • Journal of the Atmospheric Sciences

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    contributor authorSmedman, A.
    contributor authorHögström, U.
    contributor authorSahleé, E.
    contributor authorDrennan, W. M.
    contributor authorKahma, K. K.
    contributor authorPettersson, H.
    contributor authorZhang, F.
    date accessioned2017-06-09T16:28:09Z
    date available2017-06-09T16:28:09Z
    date copyright2009/09/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-68420.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209976
    description abstractBy combining simultaneous data from an instrumented Air?Sea Interaction Spar (ASIS) buoy and a 30-m tower, profiles of wind and turbulence characteristics have been obtained at several heights from about 1 to 30 m above the water surface during swell conditions. Five cases formed as averages over time periods ranging from 2.5 to 9.5 h, representing quasi-steady conditions, have been selected. They represent a range of typical wave age and include wind-following swell cases and cross-swell cases. For relatively large wave age, the wind profile exhibits a well-defined maximum in the height range 5?10 m; for more modest wave age, this maximum turns into a sharp ?knee? in the wind profile. Below the maximum (or knee), the wind increases rapidly with height; above that point the wind is very nearly constant up to the highest measuring level on the tower, 30 m. Analysis of balloon data from one day with swell indicates that the layer with constant wind in fact extends to the top of the boundary layer, in this case ?200 m. Analysis of the complete swell dataset from the 45 days of the 2003 Baltic Swell experiment shows that the results concerning wind profile shape obtained from the selected cases are generally valid in this experiment. Analysis of the nondimensional wind profile ?m shows that Monin?Obukhov scaling is not valid during swell. Wind and turbulence characteristics are found not to vary to a significant degree with the wind/swell angle within the range of angles encountered, ±90°.
    publisherAmerican Meteorological Society
    titleObservational Study of Marine Atmospheric Boundary Layer Characteristics during Swell
    typeJournal Paper
    journal volume66
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2009JAS2952.1
    journal fristpage2747
    journal lastpage2763
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009
    contenttypeFulltext
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    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