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

Title: Generation of shock/discontinuity compound structures through magnetic reconnection in the geomagnetic tail

Journal Article · · Physics of Plasmas
DOI:https://doi.org/10.1063/1.4772782· OSTI ID:22072655
 [1];  [2];  [3];  [4]
  1. Department of Physics, National Cheng Kung University, Tainan 701, Taiwan (China)
  2. Chemical Systems Research Division, Chung-Shan Institute of Science and Technology, Longtan 325, Taiwan (China)
  3. Institute of Earth Science, Academia Sinica, Nankang 115, Taiwan (China)
  4. Institute of Space Science, National Central University, Jungli 320, Taiwan (China)

We use 1-D hybrid code to simulate the generation and evolution of MHD discontinuities associated with magnetic reconnection in a current sheet. It is found that the leakage of slow shock (SS) downstream particles to upstream region tends to increase the ion parallel temperature and temperature anisotropy with {beta}{sub i||}/{beta}{sub i Up-Tack } Much-Greater-Than 1, where {beta}{sub i||}({beta}{sub i Up-Tack }) is the ion parallel (perpendicular) beta. As a result, the propagation speed of rotational discontinuity (RD) is highly reduced and RD becomes attached to SS, leading to formation of various compound structures in the reconnection outflow region. Four types of compound structure are found in our simulations: (a) RD-SS compound structure: the RD is attached to the leading part of SS, (b) SS-RD (DD) compound structure: RD is attached to the rear part of SS, (c) SS-RD-SS compound structure: RD is trapped inside SS, and (d) switch-off slow shock (SSS) with a rotational wave train. The type of compound structure generated depends on initial ion beta {beta}{sub i0} and magnetic shear angle {phi}. RD tends to move in front of SS to form an RD-SS compound structure for cases with low {beta}{sub i0}. RD stays behind SS and form an SS-RD (DD) compound structure for large {beta}{sub i0}. The SS-RD-SS compound structure is formed for intermediate values of {beta}{sub i0}. When the shear angle is 180 Degree-Sign , SSS with a wave train is formed.

OSTI ID:
22072655
Journal Information:
Physics of Plasmas, Vol. 19, Issue 12; Other Information: (c) 2012 American Institute of Physics; Country of input: International Atomic Energy Agency (IAEA); ISSN 1070-664X
Country of Publication:
United States
Language:
English

Similar Records

Evolution of symmetric reconnection layer in the presence of parallel shear flow
Journal Article · Fri Jul 15 00:00:00 EDT 2011 · Physics of Plasmas · OSTI ID:22072655

Hybrid simulations of intermediate shocks: Coplanar and noncoplanar solutions
Journal Article · Fri Sep 04 00:00:00 EDT 1992 · Geophysical Research Letters (American Geophysical Union); (United States) · OSTI ID:22072655

Observation of anomalous slow-mode shock and reconnection layer in the dayside magnetopause
Journal Article · Thu Dec 01 00:00:00 EST 1994 · Journal of Geophysical Research · OSTI ID:22072655