MHD Simulations of SIs observed by Polar

Other

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

2730 Magnetosphere: Inner, 2731 Magnetosphere: Outer, 2753 Numerical Modeling, 2784 Solar Wind/Magnetosphere Interactions

Scientific paper

We use the UCLA MHD Geospace General Circulation Model (GGCM) to simulate Sudden Impulses (SI) observed by the Magnetic Field Experiment (MFE) onboard Polar. SI's are observable on the surface of the Earth as abrupt changes in the magnetic field magnitude caused by thin solar wind discontinuities across which the solar wind dynamic pressure abruptly and significantly increases. They compress the magnetosphere as they move past the Earth. The empirical T89 and T96 models developed by N. Tsyganenko can be used to predict the steady state changes in field magnitude but an MHD model can also resolve the temporal evolution of the SI signal. Since the rise time of an SI is used to determine the distance a shock travels along the length of the magnetosphere the MHD model is more useful for predicting such an occurrence. By varying the speed of a shock, and other solar wind parameters, we investigate the respective effect that various parameters have on the rise time and magnitude of an SI.

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

MHD Simulations of SIs observed by Polar 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 MHD Simulations of SIs observed by Polar, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and MHD Simulations of SIs observed by Polar will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1651637

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