Theory and observation of electromagnetic ion cyclotron triggered emissions in the magnetosphere
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- Yoshiharu Omura
- Research Institute for Sustainable Humanosphere Kyoto University Kyoto Japan
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- Jolene Pickett
- Department of Physics and Astronomy University of Iowa Iowa City Iowa USA
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- Benjamin Grison
- Institute of Atmospheric Physics Academy of Sciences of the Czech Republic Prague Czech Republic
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- Ondrej Santolik
- Institute of Atmospheric Physics Academy of Sciences of the Czech Republic Prague Czech Republic
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- Iannis Dandouras
- Centre d'Etude Spatiale des Rayonnements Université de Toulouse Toulouse France
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- Mark Engebretson
- Department of Physics Augsburg College Minneapolis Minnesota USA
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- Pierrette M. E. Décréau
- Laboratoire de Physique et Chimie de l'Environnement et de l'Espace, UMR 6115 Université d'Orléans, CNRS Orleans France
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- Arnaud Masson
- Science Operations Department European Space Agency Noordwijk Netherlands
書誌事項
- 公開日
- 2010-07
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2010ja015300
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:p>We develop a nonlinear wave growth theory of electromagnetic ion cyclotron (EMIC) triggered emissions observed in the inner magnetosphere. We first derive the basic wave equations from Maxwell's equations and the momentum equations for the electrons and ions. We then obtain equations that describe the nonlinear dynamics of resonant protons interacting with an EMIC wave. The frequency sweep rate of the wave plays an important role in forming the resonant current that controls the wave growth. Assuming an optimum condition for the maximum growth rate as an absolute instability at the magnetic equator and a self‐sustaining growth condition for the wave propagating from the magnetic equator, we obtain a set of ordinary differential equations that describe the nonlinear evolution of a rising tone emission generated at the magnetic equator. Using the physical parameters inferred from the wave, particle, and magnetic field data measured by the Cluster spacecraft, we determine the dispersion relation for the EMIC waves. Integrating the differential equations numerically, we obtain a solution for the time variation of the amplitude and frequency of a rising tone emission at the equator. Assuming saturation of the wave amplitude, as is found in the observations, we find good agreement between the numerical solutions and the wave spectrum of the EMIC triggered emissions.</jats:p>
収録刊行物
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- Journal of Geophysical Research: Space Physics
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Journal of Geophysical Research: Space Physics 115 (A7), A7-, 2010-07
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1361981470386559232
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- HANDLE
- 11104/0195462
- 2433/146730
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- ISSN
- 01480227
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- データソース種別
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- Crossref
- OpenAIRE