Investigation of EMIC wave scattering as the cause for the BARREL 17 January 2013 relativistic electron precipitation event: A quantitative comparison of simulation with observations
-
- Zan Li
- Department of Physics and Astronomy Dartmouth College Hanover New Hampshire USA
-
- Robyn M. Millan
- Department of Physics and Astronomy Dartmouth College Hanover New Hampshire USA
-
- Mary K. Hudson
- Department of Physics and Astronomy Dartmouth College Hanover New Hampshire USA
-
- Leslie A. Woodger
- Department of Physics and Astronomy Dartmouth College Hanover New Hampshire USA
-
- David M. Smith
- Physics Department and Santa Cruz Institute for Particle Physics University of California Santa Cruz California USA
-
- Yue Chen
- Los Alamos National Laboratory Los Alamos New Mexico USA
-
- Reiner Friedel
- Los Alamos National Laboratory Los Alamos New Mexico USA
-
- Juan V. Rodriguez
- Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder Boulder Colorado USA
-
- Mark J. Engebretson
- Department of Physics Augsburg College Minneapolis Minnesota USA
-
- Jerry Goldstein
- Southwest Research Institute San Antonio Texas USA
-
- Joseph F. Fennell
- Space Science Applications Laboratory Aerospace Corporation Los Angeles California USA
-
- Harlan E. Spence
- Institute for the Study of Earth, Oceans, and Space University of New Hampshire Durham New Hampshire USA
書誌事項
- 公開日
- 2014-12-23
- 権利情報
-
- http://creativecommons.org/licenses/by-nc-nd/4.0/
- DOI
-
- 10.1002/2014gl062273
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:title>Abstract</jats:title><jats:p>Electromagnetic ion cyclotron (EMIC) waves were observed at multiple observatory locations for several hours on 17 January 2013. During the wave activity period, a duskside relativistic electron precipitation (REP) event was observed by one of the Balloon Array for Radiation belt Relativistic Electron Losses (BARREL) balloons and was magnetically mapped close to Geostationary Operational Environmental Satellite (GOES) 13. We simulate the relativistic electron pitch angle diffusion caused by gyroresonant interactions with EMIC waves using wave and particle data measured by multiple instruments on board GOES 13 and the Van Allen Probes. We show that the count rate, the energy distribution, and the time variation of the simulated precipitation all agree very well with the balloon observations, suggesting that EMIC wave scattering was likely the cause for the precipitation event. The event reported here is the first balloon REP event with closely conjugate EMIC wave observations, and our study employs the most detailed quantitative analysis on the link of EMIC waves with observed REP to date.</jats:p>
収録刊行物
-
- Geophysical Research Letters
-
Geophysical Research Letters 41 (24), 8722-8729, 2014-12-23
American Geophysical Union (AGU)

