Upstream particle spatial gradients and plasma waves

The upstream electron and ion fluxes detected by our experiment on ISEE 1/2 spacecraft undergo frequent time variations, from a few seconds to minutes. Many flux variations correlate with directional changes of the interplanetary magnetic field (IMF). Particles propagating in the upstream region acted on by the solar wind electric field creates a quasi-stationary particle pattern in space. Evidently, the spacecraft frequently crosses the boundaries of these particle patterns. Our analysis strongly suggests that the particle time variations are usually spatial variations that have been convoluted into our data. Estimates of the thickness of the particle boundaries deduced is ≳1 Larmor radius (for both the upstream electron and the ion events). Plasma waves are observed in association with the upstream particle fluxes and a correlation between the amplitudes and the particle boundaries is suggested. We will theoretically show that the ion and electron density gradients across the boundary play an important role in exciting the ion acoustic-like and plasma waves.

[1]  C. Russell,et al.  Upstream hydromagnetic waves and their association with backstreaming ion populations: ISEE 1 and 2 observations , 1981 .

[2]  T. Eastman,et al.  Plasma waves associated with energetic particles streaming into the solar wind from the earth's bow shock. Progress report for period ending jul 80 , 1980 .

[3]  C. Russell,et al.  Magnetic field orientation and suprathermal ion streams in the earth's foreshock , 1980 .

[4]  T. Eastman,et al.  Upstream particles observed in the earth's foreshock region. Report for 1977-1978 , 1980 .

[5]  K. Anderson A review of upstream and bow shock energetic-particle measurements , 1979 .

[6]  G. Parks,et al.  Thin sheets of energetic electrons upstream from the earth's bow shock , 1979 .

[7]  P. Kellogg,et al.  Electrostatic noise at the plasma frequency beyond the earth's bow shock , 1979 .

[8]  C. Russell,et al.  Association of low‐frequency waves with suprathermal ions in the upstream solar wind , 1979 .

[9]  R. Lin,et al.  Dual spacecraft observations of energetic particles in the vicinity of the magnetopause, bow shock, and the interplanetary medium , 1978 .

[10]  N. Sckopke,et al.  Observations of two distinct populations of bow shock ions in the upstream solar wind , 1978 .

[11]  P. Schultz Martian intrusions: Possible sites and implications , 1978 .

[12]  D. Gurnett,et al.  Ion-Acoustic Waves in the Solar Wind. , 1977 .

[13]  C. Meng,et al.  30- to 100-keV protons upstream from the earth's bow shock , 1974 .

[14]  J. Scudder,et al.  Electron observations in the solar wind and magnetosheath , 1973 .

[15]  W. Feldman,et al.  Solar wind heat transport in the vicinity of the Earth's bow shock , 1973 .

[16]  Masahisa Sugiura,et al.  Electron energy flux in the solar wind , 1971 .

[17]  F. Scarf,et al.  Nonthermal electrons and high‐frequency waves in the upstream solar wind, 2. Analysis and interpretation , 1971 .

[18]  F. Scarf,et al.  Nonthermal electrons and high-frequency waves in the upstream solar wind, 1. Observations , 1971 .

[19]  J. Asbridge,et al.  Outward flow of protons from the Earth's bow shock , 1968 .