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NASA NTRS · 19990056509

Nonlinear wave particle interaction in the Earth's foreshock

Abstract

The 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.

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BibTeXRIS

Mazelle, C., LeQueau, D., Meziane, K., Lin, R. P., Parks, G., Reme, H., Sanderson, T., Lepping, R. P.. 1997-12-01. Nonlinear wave particle interaction in the Earth's foreshock. https://ntrs.nasa.gov/citations/19990056509

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