HR: 0800h
AN: SM51A-1280 [Abstracts]
TI: A Kinetic Ballooning/Interchange Instability in the Magnetotail
AU: Coroniti, F V
EM: coroniti@astro.ucla.edu
AF: Department of Physics and Astronomy, University of California, 405 Hilgard Avenue, Los Angeles, CA
90095-1547
United States
AU: * Pritchett, P L
EM: pritchet@physics.ucla.edu
AF: Department of Physics and Astronomy, University of California, 405 Hilgard Avenue, Los Angeles, CA
90095-1547
United States
AB:
In the near-Earth plasma sheet, earthward convection can be
inhibited by plasma compression (the Erickson-Wolf effect),
resulting in the formation of a weakly magnetized region
from which the normal magnetic field component B_n increases
in both the tailward (x) and earthward (-x) directions.
Starting from a model plasma sheet equilibrium with B_n at
the midplane (z = 0) proportional to (1+x/L) mid-way along
the tail, 3D fully electromagnetic PIC simulations demonstrate
that a strong ballooning/interchange type instability develops
in the region of tailward increasing B_n. Unlike the classic
MHD ballooning mode, however, the kinetic instability has a
frequency which is below the ion bounce, diamagnetic, and
magnetic drift frequencies, and a cross-tail (y) wavelength
which is comparable to the ion gyroradius ρin in the
normal field (k_y ρin ≈ 2π). The spatial extent
of the mode in the x direction is initially of the order
of the B_n gradient length L; at late times, the ballooning
fingers of magnetic flux extend throughout and earthward
of the B_n gradient region. The polarization of the mode
is dominated by strong perturbations in the parallel magnetic
field and approximately anti-correlated plasma density, the
cross-tail Ey field, and the electrostatic potential.
The ion distribution develops a weak v_y perturbation, while
the x- and field-aligned flow velocities remain very small,
a consequence of the ion's gyromotion essentially averaging
the perturbed electric fields to zero. Thus the ions do not
move earthward with the inward moving fingers of magnetic flux.
The perturbed magnetic fields are generated by strong transverse
electron Hall currents which are coupled to a complex system
of field-aligned currents. The earthward speed of the flux
enhancements is typically about 400 km/s. A characteristic
signature of the mode is a local increase in B_z by about
a factor of two without any significant ion flow.
DE: 2744 Magnetotail
DE: 2764 Plasma sheet
DE: 2772 Plasma waves and instabilities (2471)
SC: SPA-Magnetospheric Physics [SM]
MN: Fall Meeting 2005