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    Energy–Vorticity Theory of Ideal Fluid Mechanics

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 007::page 2073
    Author:
    Névir, Peter
    ,
    Sommer, Matthias
    DOI: 10.1175/2008JAS2897.1
    Publisher: American Meteorological Society
    Abstract: Nambu field theory, originated by Névir and Blender for incompressible flows, is generalized to establish a unified energy?vorticity theory of ideal fluid mechanics. Using this approach, the degeneracy of the corresponding noncanonical Poisson bracket?a characteristic property of Hamiltonian fluid mechanics?can be replaced by a nondegenerate bracket. An energy?vorticity representation of the quasigeostrophic theory and of multilayer shallow-water models is given, highlighting the fact that potential enstrophy is just as important as energy. The energy?vorticity representation of the hydrostatic adiabatic system on isentropic surfaces can be written in complete analogy to the shallow-water equations using vorticity, divergence, and pseudodensity as prognostic variables. Furthermore, it is shown that the Eulerian equation of motion, the continuity equation, and the first law of thermodynamics, which describe the nonlinear evolution of a 3D compressible, adiabatic, and nonhydrostatic fluid, can be written in Nambu representation. Here, trilinear energy?helicity, energy?mass, and energy?entropy brackets are introduced. In this model the global conservation of Ertel?s potential enstrophy can be interpreted as a super-Casimir functional in phase space. In conclusion, it is argued that on the basis of the energy?vorticity theory of ideal fluid mechanics, new numerical schemes can be constructed, which might be of importance for modeling coherent structures in long-term integrations and climate simulations.
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      Energy–Vorticity Theory of Ideal Fluid Mechanics

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    contributor authorNévir, Peter
    contributor authorSommer, Matthias
    date accessioned2017-06-09T16:23:09Z
    date available2017-06-09T16:23:09Z
    date copyright2009/07/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-66926.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208316
    description abstractNambu field theory, originated by Névir and Blender for incompressible flows, is generalized to establish a unified energy?vorticity theory of ideal fluid mechanics. Using this approach, the degeneracy of the corresponding noncanonical Poisson bracket?a characteristic property of Hamiltonian fluid mechanics?can be replaced by a nondegenerate bracket. An energy?vorticity representation of the quasigeostrophic theory and of multilayer shallow-water models is given, highlighting the fact that potential enstrophy is just as important as energy. The energy?vorticity representation of the hydrostatic adiabatic system on isentropic surfaces can be written in complete analogy to the shallow-water equations using vorticity, divergence, and pseudodensity as prognostic variables. Furthermore, it is shown that the Eulerian equation of motion, the continuity equation, and the first law of thermodynamics, which describe the nonlinear evolution of a 3D compressible, adiabatic, and nonhydrostatic fluid, can be written in Nambu representation. Here, trilinear energy?helicity, energy?mass, and energy?entropy brackets are introduced. In this model the global conservation of Ertel?s potential enstrophy can be interpreted as a super-Casimir functional in phase space. In conclusion, it is argued that on the basis of the energy?vorticity theory of ideal fluid mechanics, new numerical schemes can be constructed, which might be of importance for modeling coherent structures in long-term integrations and climate simulations.
    publisherAmerican Meteorological Society
    titleEnergy–Vorticity Theory of Ideal Fluid Mechanics
    typeJournal Paper
    journal volume66
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2897.1
    journal fristpage2073
    journal lastpage2084
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 007
    contenttypeFulltext
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