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Tsurutani et al. 1984
Tsurutani, B.T., Smith, E.J., Richardson, I.G., Lepping, R.P., Jones, D.E., Zwicki, R.D. and Bame, S.J. (1984). Drift mirror mode waves in the distant (X=200 Re) magnetosheath. Geophysical Research Letters 11: doi: 10.1029/GL011i010p01102. issn: 0094-8276.

Drift mirror waves have been detected 207 Re downstream in the distant magnetosheath by instrumentation onboard ISEE-3. The MHD structures have estimated scale sizes of 4.6¿104 to 2.3¿105 km or 130 to 700 proton gyro-radii, assuming 1 keV protons. Simultaneous measurements on IMP-8 indicate that at the time of the events, the earth's magnetosphere was enveloped by a solar flare-associated interplanetary shock and driver gas. The (shocked) driver gas was characterized by an unusually low plasma density with a &Bgr; (plasma pressure/magnetic pressure) of ~0.2. From the instability criterion, &bgr;/&bgr;>1/&bgr;, the magnetosheath plasma should not go mirror-mode unstable unless the anisotropy, &bgr;/ &bgr;11 is large, >6. These unusual conditions are met by the demonstrated presence of highly anisotropic, energetic 35--384 keV ions with P/P11≈30. It is calculated that most of the plasma energy density can be due to >1 keV ions. The source of the ions is not well understood, but an appealing possibility is magnetic annihilation of the northward magnetosheath fields with southern hemisphere polar cusp magnetic fields.

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Geophysical Research Letters
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American Geophysical Union
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