- Impact of EMIC-Wave Driven Electron Precipitation on the Radiation Be…
Number of the records: 1  

Impact of EMIC-Wave Driven Electron Precipitation on the Radiation Belts and the Atmosphere

  1. 1.
    SYSNO ASEP0559270
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleImpact of EMIC-Wave Driven Electron Precipitation on the Radiation Belts and the Atmosphere
    Author(s) Hendry, Aaron (UFA-U) ORCID
    Seppälä, A. (NZ)
    Rodger, C. J. (NZ)
    Clilverd, M. A. (GB)
    Number of authors4
    Article numbere2020JA028671
    Source TitleJournal of Geophysical Research-Space Physics. - : Wiley - ISSN 2169-9380
    Roč. 126, č. 3 (2021)
    Number of pages14 s.
    Languageeng - English
    CountryUS - United States
    Keywordsatmospheric modeling ; electron precipitation ; EMIC waves ; particle interactions
    Subject RIVBL - Plasma and Gas Discharge Physics
    OECD categoryFluids and plasma physics (including surface physics)
    Method of publishingOpen access
    Institutional supportUFA-U - RVO:68378289
    UT WOS000636288800033
    EID SCOPUS85103268121
    DOI https://doi.org/10.1029/2020JA028671
    AnnotationIn recent years, there has been a growing body of direct experimental evidence demonstrating electromagnetic ion cyclotron (EMIC) waves driving energetic electron precipitation (EEP) at unexpectedly low, sub-MeV energies-as low as only a few hundred keV. EMIC-wave driven scattering at these energies has important ramifications for our understanding of not only radiation belt electron dynamics, but also the importance of EMIC-driven EEP to the chemical balance of the Earth's atmosphere. In this study, we use three experimentally derived EMIC-driven EEP flux spectra to investigate the impact of this precipitation on trapped radiation belt fluxes. In doing so, we resolve an apparent contradiction with earlier results derived from trapped electron flux populations that suggested EMIC waves only caused significant scattering at ultrarelativistic energies. We show that strong sub-MeV EEP measurements are not necessarily mutually exclusive with a strongly relativistic-only trapped flux response, as the sub-MEV peak precipitation is comparatively much smaller than the trapped population at those energies. Using a further six EEP spectra, we also demonstrate that EMIC-driven EEP can generate significant ionization of the Earth's atmosphere above 40 km, leading to the loss of mesospheric ozone. We find poor correlation between EMIC-driven EEP fluxes and geomagnetic activity proxies, such that EMIC-driven EEP is likely to be poorly specified in the forcing factors of modern coupled-climate models.
    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 Publishing2023
    Electronic addresshttps://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JA028671
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.