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    Air-Sea Transfer of Momentum, Heat and Water Determined from Profile Measurements During BOMEX

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 004::page 487
    Author:
    Paulson, C. A.
    ,
    Leavitt, E.
    ,
    Fleagle, R. G.
    DOI: 10.1175/1520-0485(1972)002<0487:ASTOMH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: One hundred forty-one simultaneous wind speed, temperature and humidity profiles measured during the Barbados Oceanographic and Meteorological Experiment (BOMEX) are analyzed. The observations were from heights 2?11 m above MSL and were made from the R/V Flip, a research vessel specially designed to be stable at sea. The wind measurements are corrected for the interference of Flip's hull with the air flow. Evaporation estimates from the profiles are in fair agreement with simultaneous estimates by the eddy-correlation method. However, the heat fluxes estimated by the two methods are in poor agreement. There appear to be diurnal variations in air temperature, sea surface temperature and stress. The flux of latent heat is large, averaging 17 mW cm?2, while the flux of sensible heat is always upward and ?1 mW cm?2.
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      Air-Sea Transfer of Momentum, Heat and Water Determined from Profile Measurements During BOMEX

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162108
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    contributor authorPaulson, C. A.
    contributor authorLeavitt, E.
    contributor authorFleagle, R. G.
    date accessioned2017-06-09T14:43:38Z
    date available2017-06-09T14:43:38Z
    date copyright1972/10/01
    date issued1972
    identifier issn0022-3670
    identifier otherams-25336.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162108
    description abstractOne hundred forty-one simultaneous wind speed, temperature and humidity profiles measured during the Barbados Oceanographic and Meteorological Experiment (BOMEX) are analyzed. The observations were from heights 2?11 m above MSL and were made from the R/V Flip, a research vessel specially designed to be stable at sea. The wind measurements are corrected for the interference of Flip's hull with the air flow. Evaporation estimates from the profiles are in fair agreement with simultaneous estimates by the eddy-correlation method. However, the heat fluxes estimated by the two methods are in poor agreement. There appear to be diurnal variations in air temperature, sea surface temperature and stress. The flux of latent heat is large, averaging 17 mW cm?2, while the flux of sensible heat is always upward and ?1 mW cm?2.
    publisherAmerican Meteorological Society
    titleAir-Sea Transfer of Momentum, Heat and Water Determined from Profile Measurements During BOMEX
    typeJournal Paper
    journal volume2
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1972)002<0487:ASTOMH>2.0.CO;2
    journal fristpage487
    journal lastpage497
    treeJournal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 004
    contenttypeFulltext
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