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    Weak and Strong Constraints Variational Data Assimilation with the NCOM-4DVAR in the Agulhas Region Using the Representer Method

    Source: Monthly Weather Review:;2017:;volume( 145 ):;issue: 005::page 1755
    Author:
    Ngodock, Hans
    ,
    Carrier, Matthew
    ,
    Smith, Scott
    ,
    Souopgui, Innocent
    DOI: 10.1175/MWR-D-16-0264.1
    Publisher: American Meteorological Society
    Abstract: he difference between the strong and weak constraints four-dimensional variational (4DVAR) analyses is examined using the representer method formulation, which expresses the analysis as the sum of a first guess and a finite linear combination of representer functions. The latter are computed analytically for a single observation under both strong and weak constraints assumptions. Even though the strong constraints representer coefficients are different from their weak constraints counterparts, that difference is unable to help the strong constraints compensate for the loss of information that the weak constraints includes. Numerical experiments carried out in the Agulhas retroflection for single and multiobservation assimilations clearly show that the weak constraint 4DVAR produces analyses that fit the observations with significantly higher accuracy than the strong constraints.
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      Weak and Strong Constraints Variational Data Assimilation with the NCOM-4DVAR in the Agulhas Region Using the Representer Method

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4231054
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    contributor authorNgodock, Hans
    contributor authorCarrier, Matthew
    contributor authorSmith, Scott
    contributor authorSouopgui, Innocent
    date accessioned2017-06-09T17:34:24Z
    date available2017-06-09T17:34:24Z
    date copyright2017/05/01
    date issued2017
    identifier issn0027-0644
    identifier otherams-87391.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231054
    description abstracthe difference between the strong and weak constraints four-dimensional variational (4DVAR) analyses is examined using the representer method formulation, which expresses the analysis as the sum of a first guess and a finite linear combination of representer functions. The latter are computed analytically for a single observation under both strong and weak constraints assumptions. Even though the strong constraints representer coefficients are different from their weak constraints counterparts, that difference is unable to help the strong constraints compensate for the loss of information that the weak constraints includes. Numerical experiments carried out in the Agulhas retroflection for single and multiobservation assimilations clearly show that the weak constraint 4DVAR produces analyses that fit the observations with significantly higher accuracy than the strong constraints.
    publisherAmerican Meteorological Society
    titleWeak and Strong Constraints Variational Data Assimilation with the NCOM-4DVAR in the Agulhas Region Using the Representer Method
    typeJournal Paper
    journal volume145
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-16-0264.1
    journal fristpage1755
    journal lastpage1764
    treeMonthly Weather Review:;2017:;volume( 145 ):;issue: 005
    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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