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Observations and Fokker-Planck Simulations of the L-Shell, Energy, and Pitch Angle Structure of Earth's Electron Radiation Belts During Quiet Times

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    SYSNO ASEP0503901
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleObservations and Fokker-Planck Simulations of the L-Shell, Energy, and Pitch Angle Structure of Earth's Electron Radiation Belts During Quiet Times
    Author(s) Ripoll, J.-F. (FR)
    Loridan, V. (FR)
    Denton, M. H. (US)
    Cunningham, G. (US)
    Reeves, G. (US)
    Santolík, Ondřej (UFA-U) RID, ORCID
    Fennell, J. (US)
    Turner, D. L. (US)
    Drozdov, A.Y. (US)
    Cervantes Villa, J.S. (DE)
    Shprits, Y. Y. (US)
    Thaller, S. A. (US)
    Kurth, W. S. (US)
    Kletzing, C. A. (US)
    Henderson, M. G. (US)
    Ukhorskiy, A. Y. (US)
    Number of authors16
    Source TitleJournal of Geophysical Research-Space Physics. - : Wiley - ISSN 2169-9380
    Roč. 124, č. 2 (2019), s. 1125-1142
    Number of pages18 s.
    Publication formPrint - P
    Languageeng - English
    CountryUS - United States
    Keywordsradiation belts ; wave-particle interactions ; electron lifetime ; pitch angle diffusion coefficient ; hiss waves
    Subject RIVBL - Plasma and Gas Discharge Physics
    OECD categoryFluids and plasma physics (including surface physics)
    Method of publishingLimited access
    Institutional supportUFA-U - RVO:68378289
    UT WOS000462015700020
    EID SCOPUS85061240672
    DOI https://doi.org/10.1029/2018JA026111
    AnnotationThe evolution of the radiation belts in L-shell (L), energy (E), and equatorial pitch angle (alpha(0)) is analyzed during the calm 11-day interval (4-15 March) following the 1 March 2013 storm. Magnetic Electron and Ion Spectrometer (MagEIS) observations from Van Allen Probes are interpreted alongside 1D and 3D Fokker-Planck simulations combined with consistent event-driven scattering modeling from whistler mode hiss waves. Three (L, E, alpha(0)) regions persist through 11 days of hiss wave scattering, the pitch angle-dependent inner belt core (L similar to <2.2 and E < 700 keV), pitch angle homogeneous outer belt low-energy core (L > similar to 5 and E similar to < 100 keV), and a distinct pocket of electrons (L similar to [4.5, 5.5] and E similar to [0.7, 2] MeV). The pitch angle homogeneous outer belt is explained by the diffusion coefficients that are roughly constant for alpha(0) similar to <60 degrees, E > 100 keV, 3.5 < L < L-pp similar to 6. Thus, observed unidirectional flux decays can be used to estimate local pitch angle diffusion rates in that region. Top-hat distributions are computed and observed at L similar to 3-3.5 and E = 100-300 keV.
    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 Publishing2020
    Electronic addresshttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2018JA026111
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