Abstract
The contribution of the directly transmitted ions to ion heating in the low-Mach number oblique shock is determined analytically. We derive approximate expressions for the pressure tensor inside the ramp of a Jow-Mach number low-β shock. In the thin shock limit the ion state equation p ∝ n3 is recovered within the ramp, which corresponds to the complete demagnetization of ions and effective one-dimensional behavior. We derive the estimate for the maximum downstream temperature of the heated ion distribution, which depends only on the magnetic compression ratio and cross-shock potential, and may be verified observationally.
Original language | English |
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Article number | 97GL02524 |
Pages (from-to) | 2511-2514 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 24 |
Issue number | 20 |
DOIs | |
State | Published - 1 Jan 1997 |
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences