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    The Coupled Boundary Layers and Air–Sea Transfer Experiment in Low Winds

    Source: Bulletin of the American Meteorological Society:;2007:;volume( 088 ):;issue: 003::page 341
    Author:
    Edson, James
    ,
    Crawford, Timothy
    ,
    Crescenti, Jerry
    ,
    Farrar, Tom
    ,
    Frew, Nelson
    ,
    Gerbi, Greg
    ,
    Plueddemann, Albert
    ,
    Trowbridge, John
    ,
    Weller, Robert
    ,
    Williams, Albert J.
    ,
    Helmis, Costas
    ,
    Hristov, Tihomir
    ,
    Shen, Lian
    ,
    Khelif, Djamal
    ,
    Jessup, Andrew
    ,
    Jonsson, Haf
    ,
    Li, Ming
    ,
    Mahrt, Larry
    ,
    Skyllingstad, Eric
    ,
    Vickers, Dean
    ,
    McGillis, Wade
    ,
    Zappa, Chris
    ,
    Stanton, Tim
    ,
    Wang, Qing
    ,
    Sullivan, Peter
    ,
    Sun, Jielun
    ,
    Wang, Shouping
    ,
    Wilkin, John
    ,
    Yue, D. K. P.
    DOI: 10.1175/BAMS-88-3-341
    Publisher: American Meteorological Society
    Abstract: The Office of Naval Research's Coupled Boundary Layers and Air?Sea Transfer (CBLAST) program is being conducted to investigate the processes that couple the marine boundary layers and govern the exchange of heat, mass, and momentum across the air?sea interface. CBLAST-LOW was designed to investigate these processes at the low-wind extreme where the processes are often driven or strongly modulated by buoyant forcing. The focus was on conditions ranging from negligible wind stress, where buoyant forcing dominates, up to wind speeds where wave breaking and Langmuir circulations play a significant role in the exchange processes. The field program provided observations from a suite of platforms deployed in the coastal ocean south of Martha's Vineyard. Highlights from the measurement campaigns include direct measurement of the momentum and heat fluxes on both sides of the air?sea interface using a specially constructed Air?Sea Interaction Tower (ASIT), and quantification of regional oceanic variability over scales of O (1?104 mm) using a mesoscale mooring array, aircraft-borne remote sensors, drifters, and ship surveys. To our knowledge, the former represents the first successful attempt to directly and simultaneously measure the heat and momentum exchange on both sides of the air?sea interface. The latter provided a 3D picture of the oceanic boundary layer during the month-long main experiment. These observations have been combined with numerical models and direct numerical and large-eddy simulations to investigate the processes that couple the atmosphere and ocean under these conditions. For example, the oceanic measurements have been used in the Regional Ocean Modeling System (ROMS) to investigate the 3D evolution of regional ocean thermal stratification. The ultimate goal of these investigations is to incorporate improved parameterizations of these processes in coupled models such as the Coupled Ocean?Atmosphere Mesoscale Prediction System (COAMPS) to improve marine forecasts of wind, waves, and currents.
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      The Coupled Boundary Layers and Air–Sea Transfer Experiment in Low Winds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4215048
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    • Bulletin of the American Meteorological Society

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    contributor authorEdson, James
    contributor authorCrawford, Timothy
    contributor authorCrescenti, Jerry
    contributor authorFarrar, Tom
    contributor authorFrew, Nelson
    contributor authorGerbi, Greg
    contributor authorPlueddemann, Albert
    contributor authorTrowbridge, John
    contributor authorWeller, Robert
    contributor authorWilliams, Albert J.
    contributor authorHelmis, Costas
    contributor authorHristov, Tihomir
    contributor authorShen, Lian
    contributor authorKhelif, Djamal
    contributor authorJessup, Andrew
    contributor authorJonsson, Haf
    contributor authorLi, Ming
    contributor authorMahrt, Larry
    contributor authorSkyllingstad, Eric
    contributor authorVickers, Dean
    contributor authorMcGillis, Wade
    contributor authorZappa, Chris
    contributor authorStanton, Tim
    contributor authorWang, Qing
    contributor authorSullivan, Peter
    contributor authorSun, Jielun
    contributor authorWang, Shouping
    contributor authorWilkin, John
    contributor authorYue, D. K. P.
    date accessioned2017-06-09T16:43:21Z
    date available2017-06-09T16:43:21Z
    date copyright2007/03/01
    date issued2007
    identifier issn0003-0007
    identifier otherams-72985.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215048
    description abstractThe Office of Naval Research's Coupled Boundary Layers and Air?Sea Transfer (CBLAST) program is being conducted to investigate the processes that couple the marine boundary layers and govern the exchange of heat, mass, and momentum across the air?sea interface. CBLAST-LOW was designed to investigate these processes at the low-wind extreme where the processes are often driven or strongly modulated by buoyant forcing. The focus was on conditions ranging from negligible wind stress, where buoyant forcing dominates, up to wind speeds where wave breaking and Langmuir circulations play a significant role in the exchange processes. The field program provided observations from a suite of platforms deployed in the coastal ocean south of Martha's Vineyard. Highlights from the measurement campaigns include direct measurement of the momentum and heat fluxes on both sides of the air?sea interface using a specially constructed Air?Sea Interaction Tower (ASIT), and quantification of regional oceanic variability over scales of O (1?104 mm) using a mesoscale mooring array, aircraft-borne remote sensors, drifters, and ship surveys. To our knowledge, the former represents the first successful attempt to directly and simultaneously measure the heat and momentum exchange on both sides of the air?sea interface. The latter provided a 3D picture of the oceanic boundary layer during the month-long main experiment. These observations have been combined with numerical models and direct numerical and large-eddy simulations to investigate the processes that couple the atmosphere and ocean under these conditions. For example, the oceanic measurements have been used in the Regional Ocean Modeling System (ROMS) to investigate the 3D evolution of regional ocean thermal stratification. The ultimate goal of these investigations is to incorporate improved parameterizations of these processes in coupled models such as the Coupled Ocean?Atmosphere Mesoscale Prediction System (COAMPS) to improve marine forecasts of wind, waves, and currents.
    publisherAmerican Meteorological Society
    titleThe Coupled Boundary Layers and Air–Sea Transfer Experiment in Low Winds
    typeJournal Paper
    journal volume88
    journal issue3
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-88-3-341
    journal fristpage341
    journal lastpage356
    treeBulletin of the American Meteorological Society:;2007:;volume( 088 ):;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