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Spatial structures of magnetic depression in the Earth's high-altitude cusp: Cluster multipoint observations

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    SYSNO ASEP0333417
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleSpatial structures of magnetic depression in the Earth's high-altitude cusp: Cluster multipoint observations
    TitleProstorová struktura magnetických děr ve vzdáleném zemském cuspu: vícebodová pozorování družic Cluster
    Author(s) Shi, Q. Q. (CN)
    Pu, Z. Y. (CN)
    Souček, Jan (UFA-U) RID, ORCID
    Zong, Q. -G. (CN)
    Fu, S. Y. (CN)
    Xie, L. (CN)
    Chen, Y. (CN)
    Zhang, H. (US)
    Li, L. (CN)
    Xia, L. D. (CN)
    Liu, Z. X. (CN)
    Lucek, E. (GB)
    Fazakerley, A. N. (GB)
    Reme, H. (FR)
    Source TitleJournal of Geophysical Research - ISSN 0148-0227
    Roč. 114, - (2009), A10202/1-A10202/13
    Number of pages13 s.
    Languageeng - English
    CountryUS - United States
    Keywordshigh-altitude cusp ; mirror modes ; magnetic holes ; multi-spacecraft methods
    Subject RIVBL - Plasma and Gas Discharge Physics
    R&D ProjectsIAA301120601 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30420517 - UFA-U, BC-A (2005-2011)
    UT WOS000270707200001
    DOI10.1029/2009JA014283
    AnnotationMagnetic depression structures (magnetic holes) of short time duration from seconds to minutes have been studied using Cluster data in the high-latitude cusp. Our analysis revealed that the magnetic depressions are spatial structures traveling across the spacecraft. We show that multiple properties of the magnetic depressions are consistent with those of mirror structures observed in the magnetosheath or solar wind. The plasma in the cusp is rarely unstable with respect to mirror instability. However, as has been shown by previous studies, once a large magnetic hole is created by mirror instability, it becomes relatively stable and can survive for extended periods of time even if surrounding plasma conditions drop well below the mirror threshold. Specifically, the magnetic holes could be generated in the magnetosheath and enter the cusp due to the open geometry of the cusp magnetic field.
    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 Publishing2010
Number of the records: 1  

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