Quasi-static theory of the earth's magnetotail, including the far tail

Other

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

11

Earth Magnetosphere, Geomagnetic Tail, Magnetic Storms, Solar Wind, Pioneer 7 Space Probe, Pioneer 8 Space Probe, Two Dimensional Models

Scientific paper

In the framework of the self-consistent quasi-static theory for the time-dependent evolution of the earth's magnetotail in quiet times, a two-dimensional model is presented that describes the tail in the whole region in which it exists as a well-ordered structure. The starting point is the theory by Schindler and Birn (1982), into which a description of the distant tail is incorporated. Two models are presented, one with a neutral line at infinity, the other with a neutral line at a finite distance. In the latter case, the field structure near the neutral line is Y-shaped, and the neutral line and the point where tail flaring ends have the same x coordinate. The occurrence of large plasma bulk flow velocities at the plasma sheet boundary and their relationship with magnetic reconnection at the distant neutral line are also briefly discussed.

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

Quasi-static theory of the earth's magnetotail, including the far tail 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 Quasi-static theory of the earth's magnetotail, including the far tail, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Quasi-static theory of the earth's magnetotail, including the far tail will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1182037

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