Interplanetary magnetic field control of the Mars bow shock - Evidence for Venuslike interaction

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

14

Interplanetary Magnetic Fields, Mars (Planet), Planetary Magnetospheres, Bow Waves, Shock Waves, Venus (Planet)

Scientific paper

The Mars bow shock location and shape have been determined by examining the Phobos spacecraft magnetometer data. Observations show that the position of the terminator bow shock varies with interplanetary magnetic field orientation in the same way as at Venus. The shock is farthest from Mars in the direction of the interplanetary electric field, consistent with the idea that mass loading plays an important role in the solar wind interaction with Mars. The shock cross section at the terminator plane is asymmetric and is controlled by the interplanetary magnetic field. The shock is farther from Mars during solar maximum. Thus the solar wind interaction with Mars appears to be Venuslike, with a magnetic moment too small to affect significantly the solar wind interaction.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Interplanetary magnetic field control of the Mars bow shock - Evidence for Venuslike interaction does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Interplanetary magnetic field control of the Mars bow shock - Evidence for Venuslike interaction, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Interplanetary magnetic field control of the Mars bow shock - Evidence for Venuslike interaction will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-863202

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.