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    Observed Oceanic Variability at and near the Air-Sea Interface during Phase III of Project BOMEX

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001::page 103
    Author:
    Jacobs, Clifford A.
    DOI: 10.1175/1520-0485(1978)008<0103:OOVAAN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The natural variability observed at and near the air-sea interface during Period III of Project BOMEX is examined. The time and space variability in the observed oceanic parameters is large by classical oceanographic standards. Several interesting features were found in this BOMEX data set. Changes in the 10 m wind speed appear to be correlated to the movements of shallow temperature and salinity fronts. A secondary maximum in the mean diurnal sea surface temperature variation consistently appears in the early morning (local time). The diurnal heating patterns in the mixed layer imply a relationship between the vertical density gradient and the intensity of the vertical turbulent mixing. This relationship is further explored in numerical model studies in a companion paper (Jacobs, 1978).
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      Observed Oceanic Variability at and near the Air-Sea Interface during Phase III of Project BOMEX

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    contributor authorJacobs, Clifford A.
    date accessioned2017-06-09T14:44:43Z
    date available2017-06-09T14:44:43Z
    date copyright1978/01/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25784.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162605
    description abstractThe natural variability observed at and near the air-sea interface during Period III of Project BOMEX is examined. The time and space variability in the observed oceanic parameters is large by classical oceanographic standards. Several interesting features were found in this BOMEX data set. Changes in the 10 m wind speed appear to be correlated to the movements of shallow temperature and salinity fronts. A secondary maximum in the mean diurnal sea surface temperature variation consistently appears in the early morning (local time). The diurnal heating patterns in the mixed layer imply a relationship between the vertical density gradient and the intensity of the vertical turbulent mixing. This relationship is further explored in numerical model studies in a companion paper (Jacobs, 1978).
    publisherAmerican Meteorological Society
    titleObserved Oceanic Variability at and near the Air-Sea Interface during Phase III of Project BOMEX
    typeJournal Paper
    journal volume8
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0103:OOVAAN>2.0.CO;2
    journal fristpage103
    journal lastpage118
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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