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    On the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007::page 1776
    Author:
    Connolley, W. M.
    ,
    Gregory, J. M.
    ,
    Hunke, E.
    ,
    McLaren, A. J.
    DOI: 10.1175/1520-0485(2004)034<1776:OTCSOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The standard way in which the sea-ice dynamics equation is used in models assumes that the wind stress and ocean drag do not depend on the sea-ice concentration. It is demonstrated that this assumption is inconsistent with the free-drift limit, and how great an effect it has in practice is examined. By examining the momentum balance in the free-drift limit, the authors determine the proper area scaling for the forcing terms, thereby obtaining a more accurate solution, particularly in low-ice-concentration regions.
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      On the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4167396
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    contributor authorConnolley, W. M.
    contributor authorGregory, J. M.
    contributor authorHunke, E.
    contributor authorMcLaren, A. J.
    date accessioned2017-06-09T14:56:31Z
    date available2017-06-09T14:56:31Z
    date copyright2004/07/01
    date issued2004
    identifier issn0022-3670
    identifier otherams-30095.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167396
    description abstractThe standard way in which the sea-ice dynamics equation is used in models assumes that the wind stress and ocean drag do not depend on the sea-ice concentration. It is demonstrated that this assumption is inconsistent with the free-drift limit, and how great an effect it has in practice is examined. By examining the momentum balance in the free-drift limit, the authors determine the proper area scaling for the forcing terms, thereby obtaining a more accurate solution, particularly in low-ice-concentration regions.
    publisherAmerican Meteorological Society
    titleOn the Consistent Scaling of Terms in the Sea-Ice Dynamics Equation
    typeJournal Paper
    journal volume34
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2004)034<1776:OTCSOT>2.0.CO;2
    journal fristpage1776
    journal lastpage1780
    treeJournal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007
    contenttypeFulltext
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