Abstract
Plasma and field data from the ISEE‐3 space probe provide evidence that the lobe‐plasma sheet boundary in the central part of the distant geomagnetic tail is often a slow‐mode shock. Such shocks are predicted by Petchek's model of reconnection. If this model applies, then the ISEE‐3 observations place the general location of the reconnection diffusion region closer to the earth than x ≈ −100 RE.
Original language | English (US) |
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Pages (from-to) | 599-602 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 11 |
Issue number | 6 |
DOIs | |
State | Published - Jun 1984 |
All Science Journal Classification (ASJC) codes
- Geophysics
- General Earth and Planetary Sciences