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Title: Magnetic spectral signatures in the Earth`s magnetosheath and plasma depletion layer

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JA02827· OSTI ID:121229
 [1];  [2];  [3];  [4]
  1. Johns Hopkins Univ., Laurel, MD (United States)
  2. Lockheed Palo Alto Research Lab., CA (United States)
  3. Los Alamos National Lab., NM (United States)
  4. Dartmouth College, Hanover, NH (United States)

Correlations between plasma properties and magnetic fluctuations in the subsolar magnetosheath downstream of a quasi-perpendicular shock have been found and indicate that mirror and ion cyclotronlike fluctuations correlate with the magnetosheath proper and plasma depletion layer, respectively. The authors explore the entire range of magnetic spectral signatures observed from the AMPTE/CCE spacecraft in the magnetosheath downstream of a quasi-perpendicular shock. The magnetic spectral signatures typically progress from predominantly compressional fluctuations, {delta}B{sub {parallel}}/{delta}B{sub {perpendicular}} {approx} 3, with F/F{sub p} < 0.2 (F and F{sub p} are the wave frequency and proton gyrofrequency, respectively) to predominantly transverse fluctuations, {delta}B{sub {parallel}}/{delta}B{sub {perpendicular}} {approx} 0.3, expending up to F{sub p}. The compressional fluctuations are characterized by anticorrelation between the field magnitude and electron density, n{sub e}, and by a small compressibility, C{sub e} {triple_bond} ({delta}n{sub e}/n{sub e}){sup 2}(B/{delta}B{sub {parallel}}){sup 2} {approx} 0.13, indicative of mirror waves. The spectral characteristics of the transverse fluctuations are in agreement with predictions of linear Vlasov theory for the H{sup +} and He{sup 2+} cyclotron modes. The agreement of observed properties and predictions of local theory suggests that the spectral signatures reflect the local plasma environment and that the anisotropy instabilities regulate A{sub p}. The authors suggest that the spectral characteristics may provide a useful basis for ordering observations in the magnetosheath and that the A{sub p} - {beta}{sub {parallel}p} inverse correlation may be used as a beta-dependent upper limit on the proton anisotropy to represent kinetic effects. 32 refs., 10 figs., 2 tabs.

OSTI ID:
121229
Journal Information:
Journal of Geophysical Research, Vol. 99, Issue A4; Other Information: PBD: 1 Apr 1994
Country of Publication:
United States
Language:
English

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