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    Energy Diagnostics in a 1½-Layer, Nonisopycnic Model

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 007::page 1472
    Author:
    Røed, Lars Petter
    DOI: 10.1175/1520-0485(1997)027<1472:EDIALN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The development of a pointwise (in the horizontal) energy diagnostic scheme applicable to a 1½-layer, nonisopycnic, primitive equation model is presented. The scheme utilizes the concept of available gravitational energy to replace the conventional potential energy. This gives a total energy (kinetic plus potential) that is zero and a minimum with respect to a given reference state (a positive definite quantity) locally. Mean and eddy components of the kinetic and available gravitational energy forms are defined by introducing a thickness-weighted mean for velocity and density. Finally, mathematical formulations for the conversion terms, that is, those terms responsible for a reversible exchange of energy between the four energy compartments, are derived.
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      Energy Diagnostics in a 1½-Layer, Nonisopycnic Model

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    contributor authorRøed, Lars Petter
    date accessioned2017-06-09T14:52:38Z
    date available2017-06-09T14:52:38Z
    date copyright1997/07/01
    date issued1997
    identifier issn0022-3670
    identifier otherams-28735.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165884
    description abstractThe development of a pointwise (in the horizontal) energy diagnostic scheme applicable to a 1½-layer, nonisopycnic, primitive equation model is presented. The scheme utilizes the concept of available gravitational energy to replace the conventional potential energy. This gives a total energy (kinetic plus potential) that is zero and a minimum with respect to a given reference state (a positive definite quantity) locally. Mean and eddy components of the kinetic and available gravitational energy forms are defined by introducing a thickness-weighted mean for velocity and density. Finally, mathematical formulations for the conversion terms, that is, those terms responsible for a reversible exchange of energy between the four energy compartments, are derived.
    publisherAmerican Meteorological Society
    titleEnergy Diagnostics in a 1½-Layer, Nonisopycnic Model
    typeJournal Paper
    journal volume27
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1997)027<1472:EDIALN>2.0.CO;2
    journal fristpage1472
    journal lastpage1476
    treeJournal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 007
    contenttypeFulltext
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