論文

査読有り
2010年5月

Cluster observations of EMIC triggered emissions in association with Pc1 waves near Earth's plasmapause

GEOPHYSICAL RESEARCH LETTERS
  • J. S. Pickett
  • B. Grison
  • Y. Omura
  • M. J. Engebretson
  • I. Dandouras
  • A. Masson
  • M. L. Adrian
  • O. Santolik
  • P. M. E. Decreau
  • N. Cornilleau-Wehrlin
  • D. Constantinescu
  • 全て表示

37
9
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1029/2010GL042648
出版者・発行元
AMER GEOPHYSICAL UNION

The Cluster spacecraft were favorably positioned on the nightside near the equatorial plasmapause of Earth at L similar to 4.3 on 30 March 2002 to observe electromagnetic ion cyclotron (EMIC) rising tone emissions in association with Pc1 waves at 1.5 Hz. The EMIC rising tone emissions were found to be left-hand, circularly polarized, dispersive, and propagating away from the equator. Their burstiness and dispersion of similar to 30s/Hz rising out of the 1.5 Hz Pc1 waves are consistent with their identification as EMIC triggered chorus emissions, the first to be reported through in situ observations near the plasmapause. Along with the expected H(+) ring current ions seen at higher energies (>300 eV), lower energy ions (300 eV and less) were observed during the most intense EMIC triggered emission events. Nonlinear wave-particle interactions via cyclotron resonance between the similar to 2-10 keV H(+) ions with temperature anisotropy and the linearly-amplified Pc1 waves are suggested as a possible generation mechanism for the EMIC triggered emissions. Citation: Pickett, J. S., et al. (2010), Cluster observations of EMIC triggered emissions in association with Pc1 waves near Earth's plasmapause, Geophys. Res. Lett., 37, L09104, doi:10.1029/2010GL042648.

リンク情報
DOI
https://doi.org/10.1029/2010GL042648
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000277478100001&DestApp=WOS_CPL
ID情報
  • DOI : 10.1029/2010GL042648
  • ISSN : 0094-8276
  • Web of Science ID : WOS:000277478100001

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