Cluster Multipoint Observations of Magnetotail Current Instabilities Reveal Signatures Predicted by SIMULATION!

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

2744 Magnetotail, 2753 Numerical Modeling, 2772 Plasma Waves And Instabilities, 7835 Magnetic Reconnection

Scientific paper

Utilizing CLUSTER-multipoint observations during tail passages of the four s/c we found evidence for thin current sheet traversals. At the center of the sheet a plasma wave was found to propagate in the current direction. We compare the wave features with signatures of thin current sheet instabilities and reconnection which we obtained by kinetic plasma simulation. It appears that several instability signatures predicted by simulation can be found in CLUSTER observations. Thus the observations seem to indicate that thin current sheets develop an unstable wave mode propagating in the current direction. In the observation the current instability was followed by an outbreak of reconnection.

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

Cluster Multipoint Observations of Magnetotail Current Instabilities Reveal Signatures Predicted by SIMULATION! 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 Cluster Multipoint Observations of Magnetotail Current Instabilities Reveal Signatures Predicted by SIMULATION!, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Cluster Multipoint Observations of Magnetotail Current Instabilities Reveal Signatures Predicted by SIMULATION! will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1724217

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