Résumé
The auroral kilometric radiation (AKR) consists of a large number of fast drifting elementary radiation events that have been interpreted as travelling electron holes resulting from the nonlinear evolution of electron-acoustic waves. The elementary radiation structures sometimes become reflected or trapped in slowly drifting larger structures where the parallel electric fields are located. These latter features have spectral frequency drifts which can be interpreted in terms of the propagation of shock-like disturbances along the auroral field line at velocities near the ion-acoustic speed. The amplitude, speed, and shock width of such localized ion-acoustic shocks are determined here in the fluid approximation from the Sagdeev potential, assuming realistic plasma parameters. It is emphasized that the electrostatic potentials of such nonlinear structures contribute to auroral acceleration.
| langue originale | Anglais |
|---|---|
| Pages (de - à) | 87-92 |
| Nombre de pages | 6 |
| journal | Nonlinear Processes in Geophysics |
| Volume | 10 |
| Numéro de publication | 1-2 |
| Les DOIs | |
| état | Publié - 1 janv. 2003 |
| Modification externe | Oui |
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