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Spectral Transfer and Karman-Howarth-Monin Equations for Compressible Hall Magnetohydrodynamics

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    SYSNO ASEP0545155
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleSpectral Transfer and Karman-Howarth-Monin Equations for Compressible Hall Magnetohydrodynamics
    Author(s) Hellinger, Petr (UFA-U) RID, ORCID
    Papini, E. (IT)
    Verdini, A. (IT)
    Landi, S. (IT)
    Franci, L. (GB)
    Matteini, L. (GB)
    Montagud-Camps, V. (CZ)
    Number of authors7
    Article number101
    Source TitleAstrophysical Journal - ISSN 0004-637X
    Roč. 917, č. 2 (2021)
    Number of pages11 s.
    Languageeng - English
    CountryUS - United States
    Keywordssolar-wind turbulence ; energy-transfer ; scale dependence ; mhd turbulence ; proton ; energetics ; cascade
    Subject RIVBN - Astronomy, Celestial Mechanics, Astrophysics
    OECD categoryAstronomy (including astrophysics,space science)
    Method of publishingOpen access
    Institutional supportUFA-U - RVO:68378289
    UT WOS000687846700001
    EID SCOPUS85114419268
    DOI10.3847/1538-4357/ac088f
    AnnotationWe derive two new forms of the Karman-Howarth-Monin (KHM) equation for decaying compressible Hall magnetohydrodynamic (MHD) turbulence. We test them on results of a weakly compressible, 2D, moderate-Reynolds-number Hall MHD simulation and compare them with an isotropic spectral transfer (ST) equation. The KHM and ST equations are automatically satisfied during the whole simulation owing to the periodic boundary conditions and have complementary cumulative behavior. They are used here to analyze the onset of turbulence and its properties when it is fully developed. These approaches give equivalent results characterizing the decay of the kinetic + magnetic energy at large scales, the MHD and Hall cross-scale energy transfer/cascade, the pressure dilatation, and the dissipation. The Hall cascade appears when the MHD one brings the energy close to the ion inertial range and is related to the formation of reconnecting current sheets. At later times, the pressure dilatation energy exchange rate oscillates around zero, with no net effect on the cross-scale energy transfer when averaged over a period of its oscillations. A reduced 1D analysis suggests that all three methods may be useful to estimate the energy cascade rate from in situ observations.
    WorkplaceInstitute of Atmospheric Physics
    ContactKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Year of Publishing2022
    Electronic addresshttps://iopscience.iop.org/article/10.3847/1538-4357/ac088f
Number of the records: 1  

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