skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: A mechanism to produce a dawn-dusk component of plasma flow during magnetic reconnection in the magnetotail

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JA02269· OSTI ID:121250
; ;  [1]
  1. Univ. of Alaska, Fairbanks, AK (United States); and others

Magnetic reconnection between antiparallel field lines in the magnetotail is generally thought to produce plasma acceleration in the earthward-tailward direction. However, measurements of the plasma velocity in the magnetotail during substorm activity sometimes reveal a dawn-dusk component of plasma flow. In this paper, the authors show that a dawn-dusk component of plasma acceleration may be produced during reconnection if the neutral line is not perpendicular to the magnetic field. In this case, MHD simulations show that reconnection between antiparallel field lines will initially produce plasma acceleration that is nearly parallel to the neutral line because the magnetic tension force is not opposed by a pressure gradient force in this direction. As the magnetic field topology evolves to a steady state, the plasma flow direction rotates until it is nearly parallel to the plane that initially contained the antiparallel magnetic field lines before reconnection (hereafter referred to as the initial field plane). However, the time required to reach a steady state (typically several hundred seconds in the magnetotail region) may be greater than the time during which the reconnection process is active. Consequently, bursts of plasma flow with a dawn-dusk component may occur in the magnetotail. The initial acceleration along the neutral line depends on the angle ({theta}{sub B}) between the neutral line and the initial field plane, with the largest burst of plasma flow along the neutral line occurring when {theta}{sub B}=45{degrees}. 11 refs., 8 figs., 1 tab.

OSTI ID:
121250
Journal Information:
Journal of Geophysical Research, Vol. 99, Issue A4; Other Information: PBD: 1 Apr 1994
Country of Publication:
United States
Language:
English

Similar Records

Three-dimensional computer modeling of dynamic reconnection in the geomagnetic tail
Journal Article · Sat Aug 01 00:00:00 EDT 1981 · J. Geophys. Res.; (United States) · OSTI ID:121250

Magnetotail reconnection: Current diversion and field-aligned currents
Journal Article · Mon Apr 01 00:00:00 EST 1991 · Geophysical Research Letters (American Geophysical Union); (United States) · OSTI ID:121250

Evolution of flux ropes in the magnetotail: A three-dimensional global hybrid simulation
Journal Article · Fri May 15 00:00:00 EDT 2015 · Physics of Plasmas · OSTI ID:121250