An extended study of the low‐latitude boundary layer on the dawn and dusk flanks of the magnetosphere

We present a study of the low-latitude boundary layer (LLBL) using ISEE 1 energetic particle, plasma, and magnetic field data obtained during numerous traversals of the LLBL that occurred on 66 ISEE 1 passes through the magnetospheric flank LLBL region. We use energetic particle distributions to determine dawn and dusk LLBL behavior and topology for varying orientations of the magnetosheath and/or interplanetary magnetic field (M/IMF), for different local times, and for changing levels of geomagnetic activity (Kp). This study corroborates and extends the earlier work of Williams et al. (1985) who presented a detailed study of two (dusk and dawn) ISEE 1 passes through the LLBL region for the case of northward M/IMF. We find that the dawn and dusk LLBL are on closed geomagnetic field lines for northward M/IMF but are on a combination of closed and open field lines for a southward M/IMF. The energetic particle distributions show that cases of reverse-draped field lines in the LLBL are consistent with an open field line topology. In addition, we find that the LLBL is thicker (thinner) for northward (southward) M/IMF and becomes thicker with increasing distance from the subsolar point. LLBL electric fields nominally are in the few (3–5) millivolts per meter range and display an apparent maximum value of ∼10 mV/m. These electric fields capture magnetospherically drifting particles as they approach the LLBL and propel them tailward. In this way, the plasma sheet is the dominant source of energetic (≳10 keV) particles in the LLBL while the magnetosheath appears to be the dominant source for lower-energy (≲10 keV) LLBL particles.

[1]  V. Vasyliūnas,et al.  A survey of low-energy electrons in the evening sector of the magnetosphere with OGO 1 and OGO 3. , 1968 .

[2]  J. Spreiter,et al.  Plasma flow around the magnetosphere. , 1969 .

[3]  L. Frank,et al.  ELECTRON OBSERVATIONS BETWEEN THE INNER EDGE OF THE PLASMA SHEET AND THE PLASMASPHERE. Progress Report. , 1970 .

[4]  H. Rosenbauer,et al.  Heos 2 plasma observations in the distant polar magnetosphere: The plasma mantle , 1975 .

[5]  G. Paschmann,et al.  The frontside boundary layer of the magnetosphere and the problem of reconnection , 1977 .

[6]  C. Russell,et al.  The ISEE 1 and 2 Fluxgate Magnetometers , 1978, IEEE Transactions on Geoscience Electronics.

[7]  B. Wilken,et al.  The ISEE 1 and 2 Medium Energy Particles Experiment , 1978, IEEE Transactions on Geoscience Electronics.

[8]  K. Ackerson,et al.  Quadrispherical LEPEDEAS for ISEE's-1 and -2 Plasma Measurements , 1978, IEEE Transactions on Geoscience Electronics.

[9]  E. W. Hones,et al.  Characteristics of the magnetospheric boundary layer and magnetopause layer as observed by Imp 6 , 1979 .

[10]  E. W. Hones,et al.  Structure of the low‐latitude boundary layer , 1980 .

[11]  B. Sonnerup Theory of the low-latitude boundary layer , 1980 .

[12]  E. W. Hones,et al.  Reverse draping of magnetic field lines in the boundary layer , 1982 .

[13]  C. Russell,et al.  The thickness of the magnetopause current layer: ISEE 1 and 2 observations , 1982 .

[14]  T. Fritz,et al.  Trapped electron distributions on open magnetic field lines , 1982 .

[15]  E. W. Hones Magnetic structure of the boundary layer , 1983 .

[16]  A. Miura Anomalous transport by magnetohydrodynamic Kelvin‐Helmholtz instabilities in the solar wind‐magnetosphere interaction , 1984 .

[17]  F. Mozer Electric field evidence on the viscous interaction at the magnetopause , 1984 .

[18]  T. Eastman,et al.  Energetic Particle Observations in the Low‐Latitude Boundary Layer , 1985 .

[19]  R. Lundin,et al.  Analyses of convective flows and spatial gradients in energetic ion observations , 1986 .