A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause

Details A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause

Sep 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005jgra..11009223k&link_type=abstract

Journal of Geophysical Research, Volume 110, Issue A9, CiteID A09223

Physics

4

Magnetospheric Physics: Solar Wind/Magnetosphere Interactions, Magnetospheric Physics: Energetic Particles: Trapped, Magnetospheric Physics: Magnetopause And Boundary Layers, Magnetospheric Physics: Ring Current, Magnetospheric Physics: Magnetic Storms And Substorms (7954)

Scientific paper

It has been known that (untrapped) ring current particles can be lost through the dayside magnetopause into the magnetosheath, which is regarded as one of the major mechanisms contributing to the ring current decay. In this paper, we suggest that the solar wind dynamic pressure can play a significant role in the dayside loss in a new aspect. In order to show that, we have first analyzed the average characteristics of the dynamic pressure based on 95 geomagnetic storm events selected from the period 1997-2002. We find that the dynamic pressure overall enhances during the magnetic storm. The enhancement is most significant during the storm main phase compared to the prestorm and recovery phases, and it is higher for stronger storms. Using one of the most recent Tsyganenko models, T01s, we show that this enhanced dynamic pressure that pushes the magnetopause to move inward leads to a reduction of the scale length of the gradient of the magnetic field magnitude along the magnetopause. This results in the enhancement of the magnetic drift speed across the magnetopause. On the basis of the test particle orbit calculation, we explicitly show that this effect can be a significant factor for the particles to effectively cross the magnetopause. It applies to the adiabatic particles that have a relatively ``small'' gyroradius near the magnetopause compared to the magnetopause thickness. These particles cross the magnetopause by some number of the magnetic gradient drift motion, being in contrast to the particles with a relatively ``large'' gyroradius that can enter into the magnetosheath by crossing the magnetopause with less than one gyromotion. We argue that this can often apply to a substantial population of the ring current particles.

Affiliated with

Also associated with

No associations

Rating

A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause 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 A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and A new perspective on the role of the solar wind dynamic pressure in the ring current particle loss through the magnetopause will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-756618