Outer magnetosphere near midnight at quiet and disturbed times

Ogo 5 magnetic-field and energetic-electron (E > 50 kev) data are used to study both the quiet-time, steady-state configuration of the outer magnetosphere or near tail region near midnight and the disturbed time changes of this configuration. The nighttime cusp is found to be a distinct feature within the plasma sheet at quiet times but indistinguishable from the plasma sheet at disturbed times. The sequence of thinning and expansion of the plasma sheet in this region in association with the substorms is studied. The response of the plasma sheet in the near tail at ∼10 RE is found to be similar to that in the more distant tail at >20 RE. Finally, the nature of field-aligned currents flowing on the plasma-sheet boundary is investigated. Assuming infinite current sheets, the sheet current density at Ogo 5 is found to be approximately 10−2 amp m−1. At ionospheric altitudes in the auroral zone, these currents scale to 10−1 amp m−1, in good agreement with low-altitude measurements. These currents in space often appear in double or multiple sheets.

[1]  C. Meng,et al.  Energetic electrons in the plasma sheet out to 40 R sub E , 1971 .

[2]  N. Ness,et al.  Configuration of the geomagnetic tail during substorms , 1970 .

[3]  E. W. Hones,et al.  Time variations of the magnetotail plasma sheet at 18 RE Determined from concurrent observations by a pair of Vela satellites , 1971 .

[4]  C. Russell,et al.  Magnetic field variations in the near geomagnetic tail associated with weak substorm activity , 1971 .

[5]  C. Russell,et al.  Satellite studies of magnetospheric substorms on August 15, 1968: 4. Ogo 5 magnetic field observations , 1973 .

[6]  A. J. Zmuda,et al.  Characteristics of transverse magnetic disturbances observed at 1100 kilometers in the auroral oval , 1970 .

[7]  P. Cloutier,et al.  Detection of geomagnetically aligned currents associated with an auroral arc , 1970 .

[8]  D. Fairfield Average magnetic field configuration of the outer magnetosphere. , 1968 .

[9]  E. W. Hones,et al.  Characteristics of the plasma sheet in the Earth's magnetotail , 1967 .

[10]  N. Ness,et al.  CORRELATION OF MAGNETIC FIELDS AND ENERGETIC ELECTRONS ON THE IMP 1 SATELLITE , 1966 .

[11]  R. McPherron,et al.  Magnetotail changes in relation to the solar wind magnetic field and magnetospheric substorms , 1971 .

[12]  M. Kivelson,et al.  Satellite studies of magnetospheric substorms on August 15, 1968: 5. Energetic electrons, spatial boundaries, and wave‐particle interactions at Ogo 5 , 1973 .

[13]  H. I. West,et al.  Satellite studies of magnetospheric substorms on August 15, 1968: 6. Ogo 5 energetic electron observations—pitch angle distributions in the nighttime magnetosphere , 1973 .

[14]  E. W. Hones,et al.  Magnetospheric substorms in the distant magnetotail observed by Imp 3 , 1971 .

[15]  H. I. West,et al.  Satellite studies of magnetospheric substorms on August 15, 1968: 7. Ogo 5 energetic proton observations—spatial boundaries , 1973 .

[16]  A. J. Zmuda,et al.  Field‐aligned current at 1100 km in the auroral region measured by satellite , 1970 .

[17]  E. W. Hones,et al.  Simultaneous observations of an energetic electron event in the magnetotail by the Vela 3A and Imp 3 satellites: 2. , 1970 .

[18]  C. Russell,et al.  Some remarks on the position and shape of the neutral sheet , 1967 .

[19]  M. D. Montgomery Observations of electrons in the Earth's magnetotail by Vela launch 2 satellites , 1968 .