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Electrostatic waves in the bow shock at Uranus

Journal Article · · Journal of Geophysical Research; (USA)
; ; ;  [1];  [2];  [3];  [4];  [5]
  1. TRW Space and Technology Group, Redondo Beach, CA (USA)
  2. National Center for Atmospheric Research, Boulder, CO (USA)
  3. Goddard Space Flight Center, Greenbelt, MD (USA)
  4. Univ. of California, San Diego, La Jolla (USA)
  5. Univ. of Iowa, Iowa City (USA)
Electrostatic emissions measured by the Voyager 2 plasma wave detector (PWS) during the inbound crossing of the Uranian bow shock are shown to differ in some aspects from the waves measured during bow shock crossings at Jupiter and Saturn. The wave amplitudes in the foot of the bow shock at Uranus are in general much lower than those detected at the other out planets due to the unusually enhanced solar wind ion temperature during the crossing. This reduces the effectiveness of wave-particle interactions in heating the incoming electrons. Strong wave emissions are observed in the shock ramp that possibly arise from currents producing a Buneman mode instability. Plasma instrument (PLS) and magnetometer (MAG) measurements reveal a complicated shock structure reminiscent of computer simulations of high-Mach number shocks when the effects of anomalous resistivity are reduced, and are consistent with high ion temperatures restricting the growth of electrostatic waves.
OSTI ID:
6051100
Journal Information:
Journal of Geophysical Research; (USA), Journal Name: Journal of Geophysical Research; (USA) Vol. 94:A10; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English

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