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Non-stationarity of the quasi-perpendicular bow shock: comparison between Cluster observations and simulations

  1. 1.
    SYSNO ASEP0360928
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleNon-stationarity of the quasi-perpendicular bow shock: comparison between Cluster observations and simulations
    Author(s) Comisel, H. (RO)
    Scholer, M. (DE)
    Souček, Jan (UFA-U) RID, ORCID
    Matsukiyo, S. (JP)
    Source TitleAnnales Geophysicae. - : Copernicus - ISSN 0992-7689
    Roč. 29, č. 2 (2011), s. 263-274
    Number of pages12 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsbow shock ; Cluster ; plasma waves ; shock waves
    Subject RIVBL - Plasma and Gas Discharge Physics
    CEZAV0Z30420517 - UFA-U, BC-A (2005-2011)
    UT WOS000287800700005
    DOI10.5194/angeo-29-263-2011
    AnnotationWe performed full particle electromagnetic simulations of a quasi-perpendicular shock with parameters corresponding to the Earth's bow shock observed by Cluster on 24 January 2001. In run 1, modified two-stream instability (MTSI) is excited by the reflected solar wind ions. The waves due to the MTSI are on the whistler mode branch and have downstream directed phase velocities in the shock frame. The Poynting flux far upstream in the foot is also directed downstream. However, in the density and magnetic field compression region of the overshoot the waves are refracted and the Poynting flux in the shock frame points upstream. The MTSI is suppressed in the low mass ratio run 2, where significant reformation (“breathing”) is observed. It is suggested that the high frequency upstream waves are due to the MTSI and are not related to a nonlinear phase standing whistler. Different profiles observed by different Cluster spacecraft are due to the non-stationary behavior on a larger time scale.
    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 Publishing2012
    Electronic addresshttp://www.ann-geophys.net/29/263/2011/angeo-29-263-2011.pdf
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