Abstract
Three discontinuities within a large disturbance of the interplanetary field, observed at Venus and previously suggested to be due to the possible passage of a comet, are examined to see if they could possibly represent the first observation of a cometary shock. The changes in number density, temperature and velocity as well as the magnetic structure of the discontinuities are consistent with this hypothesis.
Original language | English |
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Pages (from-to) | 1022-1025 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 11 |
Issue number | 10 |
DOIs | |
State | Published - Oct 1984 |