Abstract
We have calculated the proton and the oxygen velocities in the nightside magnetosheath of Mars utilising the particle observations made by ASPERA onboard the Phobos 2 spacecraft. The O+ observations can be divided into three classes according to the velocities and locations: the "central tail", the "energetic", and the "slowly moving" O+ ions. A detailed study of the energetic O+ ions shows that they are related to non-typical magnetic field conditions.
Original language | English |
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Pages (from-to) | 119-122 |
Number of pages | 4 |
Journal | Advances in Space Research |
Volume | 16 |
Issue number | 4 |
DOIs | |
Publication status | Published - 1995 |
MoE publication type | A1 Journal article-refereed |