Abstract
Electric field measurements from a single spacecraft have been used to study ion-sound turbulence observed within the Earth's bow shock. The observed frequency of the ion-sound waves can be both lower and higher than the local electron cyclotron frequency depending upon the direction of wave propagation in the plasma rest frame. The ion-sound waves observed upstream of the ramp can not be generated either by an instability related to the gradient in the electron temperature or an electric current within the ramp. A comparison of wave vectors for distinctive wave packets indicate that non-stationary, short scale current layers formed in the processes of the ramp evolution might be the source of the free energy for such waves.
Original language | English |
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Pages (from-to) | 1-4 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 32 |
Issue number | 24 |
DOIs | |
State | Published - 28 Dec 2005 |
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences