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

Journal Article · Fri Apr 01 04:00:00 EST 1994 · Journal of Geophysical Research

DOI:https://doi.org/10.1029/93JA02827· OSTI ID:121229

Anderson, B J ^[1]; Fuselier, S A ^[2]; Gary, S P ^[3]; Denton, R E ^[4]

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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, Journal Name: Journal of Geophysical Research Journal Issue: A4 Vol. 99; ISSN JGREA2; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

66 PHYSICS
ENERGY SPECTRA
FLUCTUATIONS
GEOMAGNETIC FIELD
MAGNETOSHEATH
SHOCK WAVES