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GEOPHYSICAL RESEARCH LETTERS,
VOL. 25, NO. 14,
PAGES 2613–2616,
1998
A Pair of Forward and Reverse Slow-Mode Shocks Detected by Ulysses at ∼ 5 AU
C. M. Ho
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
B. T. Tsurutani
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
N. Lin
School of Physics and Astronomy, University of Minnesota, Minneapolis, MN 55455
L. J. Lanzerotti
Bell Laboratories, Lucent Technologies, Murray Hill, NJ 07974
E. J. Smith
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
B. E. Goldstein
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
B. Buti
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
G. S. Lakhina
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
X. Y. Zhou
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109
Abstract
We report the first finding of a pair of forward and reverse slow-mode shocks in the distant heliosphere using plasma and
magnetic field data from the Ulysses spacecraft located at 5.3 AU and 9° S heliolatitude. The slow-mode shocks are found to
occur in a compressed magnetic field (low plasma ) region within a co-rotating interaction region (CIR). We find Mach numbers
to be 0.3-0.5 with respect to forward/reverse slow shocks. Across each shock, the solar wind velocities jump by at least 40
km/s. The increases in plasma density and ion temperature accompany a decrease in the magnetic field. The shocks are also
found to have velocities of 60 km/s and 115 km/s and thicknesses between 7.5 - 12.6 × 104 km (much larger than the ion inertial length, ∼ 10³ km). Low frequency plasma waves are detected by the Ulysses URAP instrument
at the slow-mode shock transition regions. However, the waves are not of sufficient amplitude to provide enough anomalous
resistivity through wave-particle interactions for shock dissipation. Low energy (∼30 - 90 keV) electron enhancements directed
along the local magnetic field are also found associated with the slow shocks, indicating the ability of the shocks to accelerate
interplanetary particles. This finding imply that more slow shocks might be found in the CIR magnetic compressed regions (where
plasma is squeezed out) at large heliospheric distances.
Received 2
March
1998;
accepted 3
June
1998.
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Citation: Ho, C. M., B. T. Tsurutani, N. Lin, L. J. Lanzerotti, E. J. Smith, B. E. Goldstein, B. Buti, G. S. Lakhina, and X. Y. Zhou
(1998),
A Pair of Forward and Reverse Slow-Mode Shocks Detected by Ulysses at ∼ 5 AU,
Geophys. Res. Lett.,
25(14),
2613–2616.
Copyright 1998 by the American Geophysical Union.
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