Current-driven lower hybrid waves at the inner edge of the ring current
Creators
- 1. Institut fuer extraterrestrische Physik, Max-Planck-Institut fuer Physik und Astrophysik, Garching bei Muenchen, Federal Republic of Germany
Description
Waves near the lower hybrid frequency have been observed in association with the diamagnetic current at the inner edge of the ring current (LaBelle et al., this issue). Here we interpret these waves in terms of the modified-two-stream instability, generalized to include two ion components: the cold ions of the background plasma and the hot drifting ring current ions. Solution of the dispersion relation yields a weak instability. Since the waves are Landau damped by the background ions, the instability depends sensitively on the background ion temperature as well as the drift velocity. The general characteristics of the observed waves are determined fairly well by the linear theory. Estimates of the saturation level suggest that the waves saturate due to flattening of the current ion distribution function. copyright American Geophysical Union 1988
Additional details
Publishing Information
- Journal Title
- J. Geophys. Res.
- Journal Volume
- 93
- Journal Issue
- A4
- Series
- J. Geophys. Res.
- Journal Page Range
- 2591-2598
- ISSN
- 0148-0227
- CODEN
- JGREA
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 19082582
- Subject category
- S58: GEOSCIENCES;
- Descriptors DEI
- DISPERSION RELATIONS; DRIFT INSTABILITY; EARTH MAGNETOSPHERE; HYBRID RESONANCE; ION DRIFT; ION PLASMA WAVES; LANDAU DAMPING; PLASMA DRIFT; RING CURRENTS; TWO-STREAM INSTABILITY
- Descriptors DEC
- CURRENTS; DAMPING; EARTH ATMOSPHERE; ELECTRIC CURRENTS; INSTABILITY; ION WAVES; PLASMA INSTABILITY; PLASMA MICROINSTABILITIES; PLASMA WAVES; RESONANCE