ISEE 1 and 2 observations of Birkeland currents in the Earth's inner magnetosphere

Data from the ISEE 1 and 2 magnetometers were examined for evidence of Birkeland currents in the earth's inner magnetosphere, from 2.4- to 7-RE radial distance. This survey reports on the two spacecraft measurements of the properties of the Birkeland currents. Both line and sheetlike currents were observed. Large-scale Birkeland current signatures were observed throughout the 18 hours of local time in which the data coverage was sufficient. In local time this coverage was from local noon through dusk to local midnight to the dawn meridian. In approximately 27% of the spacecraft's outbound passes, large-scale current structures were identifiable as parts of the region 1 or region 2 current systems. In approximately 19% of the outbound passes, no distinguishable region 1 or region 2 Birkeland currents were observed. These cases occurred during periods of low magnetic activity. In the remaining 54%, both multiple current structures and ambiguous magnetic signatures were observed. The multiple structures were generally of smaller scale than the structures identified as the region 1 and 2 current structures, and the ambiguous cases had no clear sources or causes. For these cases the spatial and temporal variations were not easily separated. Two passes through the dayside magnetosphere showed Birkeland current layers at the interface between the outer plasma sheet convection boundary and a plasma mantlelike boundary region, located inside the postnoon magnetopause. These two cases provided clear examples of region 1 Birkeland current flow in the dayside magnetosphere.

[1]  C. Russell,et al.  Observations of field‐aligned currents at the plasma sheet boundary: An ISEE‐1 and 2 survey , 1985 .

[2]  C. Russell,et al.  ISEE 1 and 2 observations of an oscillating outward moving current sheet near midnight , 1984 .

[3]  D. Stern The origins of Birkeland currents , 1983 .

[4]  Nikolai A. Tsyganenko,et al.  Determination of the magnetospheric current system parameters and development of experimental geomagnetic field models based on data from IMP and HEOS satellites , 1982 .

[5]  Robert L. McPherron,et al.  Field‐aligned currents in the Earth's magnetotail , 1981 .

[6]  D. Klumpar Relationships between auroral particle distributions and magnetic field perturbations associated with field-aligned currents , 1979 .

[7]  T. Potemra Current systems in the Earth's magnetosphere: A Review of U.S. Progress for the 1975–1978 IUGG Quadrennial Report , 1979 .

[8]  T. Potemra,et al.  Large‐scale characteristics of field‐aligned currents associated with substorms , 1978 .

[9]  D. Klumpar,et al.  Simultaneous observations of field-aligned currents and particle fluxes in the rost-midnight sector , 1976 .

[10]  T. Potemra,et al.  The amplitude distribution of field-aligned currents at northern high latitudes observed by TRIAD. Interim report , 1975 .

[11]  M. Sugiura Identifications of the polar cap boundary and the auroral belt in the high‐altitude magnetosphere: A model for field‐aligned currents , 1975 .

[12]  D. Fairfield Magnetic field signatures of substorms on high-latitude field lines in the nighttime magnetosphere , 1973 .

[13]  Robert L. McPherron,et al.  Outer magnetosphere near midnight at quiet and disturbed times , 1972 .

[14]  L. Frank Relationship of the plasma sheet, ring current, trapping boundary, and plasmapause near the magnetic equator and local midnight , 1971 .

[15]  L. J. Cahill,et al.  Explorer 12 observations of the magnetopause current layer , 1968 .

[16]  Edward J. Smith,et al.  Power spectra and discontinuities of the interplanetary magnetic field - Mariner 4. , 1968 .