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Nonlinear wave particle interaction in the Earth's foreshockThe possibility that ion beams could provide a free energy source for driving an ion/ion instability responsible for the ULF wave occurrence is investigated. For this, the wave dispersion relation with the observed parameters is solved. Secondly, it is shown that the ring-like distributions could then be produced by a coherent nonlinear wave-particle interaction. It tends to trap the ions into narrow cells in velocity space centered around a well-defined pitch-angle, directly related to the saturation wave amplitude in the analytical theory. The theoretical predictions with the observations are compared.
Document ID
19990056509
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Mazelle, C.
(Centre d'Etude Spatiale des Rayonnements Toulouse France)
LeQueau, D.
(Centre d'Etude Spatiale des Rayonnements Toulouse France)
Meziane, K.
(California Univ. Berkeley, CA United States)
Lin, R. P.
(California Univ. Berkeley, CA United States)
Parks, G.
(Washington Univ. Seattle, WA United States)
Reme, H.
(Centre d'Etude Spatiale des Rayonnements Toulouse France)
Sanderson, T.
(European Space Agency. European Space Research and Technology Center, ESTEC Noordwijk Netherlands)
Lepping, R. P.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Date Acquired
August 19, 2013
Publication Date
December 1, 1997
Publication Information
Publication: Proceedings of the 31st ESALB Symposium on Correlated Phenomena at the Sun, in the Heliosphere and in Geospace
Subject Category
Plasma Physics
Distribution Limits
Public
Copyright
Other
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