Physics
Scientific paper
Dec 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agufmsm41b0791f&link_type=abstract
American Geophysical Union, Fall Meeting 2001, abstract #SM41B-0791
Physics
2724 Magnetopause, Cusp, And Boundary Layers, 7827 Kinetic And Mhd Theory, 7839 Nonlinear Phenomena, 7859 Transport Processes, 7867 Wave/Particle Interactions
Scientific paper
The magnetopause and boundary layer are typically characterized by large amplitude transverse wave activity with freqencies below the ion cyclotron frequency. The signatures of the transverse waves suggest that they are kinetic Alfveń waves with wavelength on the order of the ion gyroradius [Johnson and Cheng, Geophys. Res. Lett., 28, 227, (2001)]. We investigate ion motion in the presence of large amplitude kinetic Alfveń waves with wavelength the order of ρ i and demonstrate that for sufficiently large wave amplitude the particle orbits become stochastic leading to ion heating and plasma transport. Low energy particles in the core of the ion distribution can migrate to higher energy through the stochastic sea leading to an increase in Tperpendicular to and a broadening of the distribution. This process can explain transverse ion energization and formation of conics which have been observed near the magnetopause in both the magnetosheath and low-latitude boundary layer. Similarly, stochastic ion transport can also occur leading to magnetosheath ion entry across the magnetopause with D ~ 109 m2/s.
Cheng C. Z.
Fu Gang
Johnson Jay Robert
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