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    Vertical Structure of Ocean Pressure Variations with Application to Satellite-Gravimetric Observations

    Source: Journal of Atmospheric and Oceanic Technology:;2014:;volume( 032 ):;issue: 003::page 603
    Author:
    Piecuch, Christopher G.
    ,
    Fukumori, Ichiro
    ,
    Ponte, Rui M.
    ,
    Wang, Ou
    DOI: 10.1175/JTECH-D-14-00156.1
    Publisher: American Meteorological Society
    Abstract: he nature of ocean bottom pressure variability is considered on large spatial scales and long temporal scales. Monthly gridded estimates from the Gravity Recovery and Climate Experiment (GRACE) Release-05 and the new version 4 bidecadal ocean state estimate of the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO) are used. Estimates of from GRACE and ECCO are generally in good agreement, providing an independent measure of the quality of both products. Diagnostic fields from the state estimate are used to compute barotropic (depth independent) and baroclinic (depth dependent) components. The relative roles of baroclinic and barotropic processes are found to vary with latitude and time scale: variations in at higher latitudes and shorter periods are affected by barotropic processes, whereas fluctuations at lower latitudes and longer periods can be influenced by baroclinic effects, broadly consistent with theoretical scaling arguments. Wind-driven Rossby waves and coupling of baroclinic and barotropic modes due to flow?topography interactions appear to be important influences on the baroclinic variability. Decadal simulations of monthly variability based on purely barotropic frameworks are expected to be in error by about 30% on average ( in the tropical ocean and at higher latitudes). Results have implications for applying GRACE observations to problems such as estimating transports of the Antarctic Circumpolar Current.
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      Vertical Structure of Ocean Pressure Variations with Application to Satellite-Gravimetric Observations

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    contributor authorPiecuch, Christopher G.
    contributor authorFukumori, Ichiro
    contributor authorPonte, Rui M.
    contributor authorWang, Ou
    date accessioned2017-06-09T17:25:59Z
    date available2017-06-09T17:25:59Z
    date copyright2015/03/01
    date issued2014
    identifier issn0739-0572
    identifier otherams-85161.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228577
    description abstracthe nature of ocean bottom pressure variability is considered on large spatial scales and long temporal scales. Monthly gridded estimates from the Gravity Recovery and Climate Experiment (GRACE) Release-05 and the new version 4 bidecadal ocean state estimate of the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO) are used. Estimates of from GRACE and ECCO are generally in good agreement, providing an independent measure of the quality of both products. Diagnostic fields from the state estimate are used to compute barotropic (depth independent) and baroclinic (depth dependent) components. The relative roles of baroclinic and barotropic processes are found to vary with latitude and time scale: variations in at higher latitudes and shorter periods are affected by barotropic processes, whereas fluctuations at lower latitudes and longer periods can be influenced by baroclinic effects, broadly consistent with theoretical scaling arguments. Wind-driven Rossby waves and coupling of baroclinic and barotropic modes due to flow?topography interactions appear to be important influences on the baroclinic variability. Decadal simulations of monthly variability based on purely barotropic frameworks are expected to be in error by about 30% on average ( in the tropical ocean and at higher latitudes). Results have implications for applying GRACE observations to problems such as estimating transports of the Antarctic Circumpolar Current.
    publisherAmerican Meteorological Society
    titleVertical Structure of Ocean Pressure Variations with Application to Satellite-Gravimetric Observations
    typeJournal Paper
    journal volume32
    journal issue3
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH-D-14-00156.1
    journal fristpage603
    journal lastpage613
    treeJournal of Atmospheric and Oceanic Technology:;2014:;volume( 032 ):;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
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