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    Stochastic Dynamic Analysis of Polar Sea Ice Variability

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 012::page 2100
    Author:
    Lemke, P.
    ,
    Trinkl, E. W.
    ,
    Hasselmann, K.
    DOI: 10.1175/1520-0485(1980)010<2100:SDAOPS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The analysis of Arctic (1966?76) and Antarctic (1973?79) sea ice data is presented, and a dynamical model based on white noise atmospheric forcing, local stabilizing relaxation and lateral diffusion and advection is constructed to explain the observations. Longitudinal dependent forcing. feedback, lateral diffusion and advection parameters are derived by fitting the model to the observed cross-spectral matrix of the sea ice anomaly fields. It is inferred that diffusion and advection of sea ice anomalies play an important role in sea ice dynamics. The model advection patterns agree reasonably well with the observed ocean surface circulation in the Arctic Ocean and around Antarctica.
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      Stochastic Dynamic Analysis of Polar Sea Ice Variability

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163039
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    • Journal of Physical Oceanography

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    contributor authorLemke, P.
    contributor authorTrinkl, E. W.
    contributor authorHasselmann, K.
    date accessioned2017-06-09T14:45:44Z
    date available2017-06-09T14:45:44Z
    date copyright1980/12/01
    date issued1980
    identifier issn0022-3670
    identifier otherams-26174.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163039
    description abstractThe analysis of Arctic (1966?76) and Antarctic (1973?79) sea ice data is presented, and a dynamical model based on white noise atmospheric forcing, local stabilizing relaxation and lateral diffusion and advection is constructed to explain the observations. Longitudinal dependent forcing. feedback, lateral diffusion and advection parameters are derived by fitting the model to the observed cross-spectral matrix of the sea ice anomaly fields. It is inferred that diffusion and advection of sea ice anomalies play an important role in sea ice dynamics. The model advection patterns agree reasonably well with the observed ocean surface circulation in the Arctic Ocean and around Antarctica.
    publisherAmerican Meteorological Society
    titleStochastic Dynamic Analysis of Polar Sea Ice Variability
    typeJournal Paper
    journal volume10
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1980)010<2100:SDAOPS>2.0.CO;2
    journal fristpage2100
    journal lastpage2120
    treeJournal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 012
    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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