A correlative study of magnetic flux transfer in the magnetosphere

The applied magnetic flux (Phi/sub a/p) of the southward component of the interplanetary magnetic field in GSM coordinates (B/sub z//sup -/) which impinges upon the sunward magnetopause has been compared with the time integral of the auroral AL index during 56 intervals within a 3-month period in 1969 when interplanetary records from Heos 1 and Explorer 35 were available. The periods of magnetic activity chosen were those for which B/sub z/>0 and AL<20..gamma.. at the beginning and end of the interval. It was found that for these intervals, ..integral.. AL dtproportionalPhi/sub a/p with a correlation coefficient of 0.94. In addition, the empirical relationships between magnetic flux transfer, the applied southward flux, and ..integral.. AL dt arrived at by Holzer and Slavin (1978) on the basis of expansions and contractions of the forward magnetosphere observed with Ogo 5 are reexamined and improved. With these expressions describing the bulk rates of magnetic flux transfer within the magnetosphere a lower limit of 0.2 +- 0.1 on the local reconnection efficiency at the magnetopause is calculated.

[1]  G. Rostoker,et al.  RESPONSE TIME OF THE MAGNETOSPHERE TO THE INTERPLANETARY ELECTRIC FIELD. , 1972 .

[2]  Robert H. Holzworth,et al.  Mathematical representation of the auroral oval , 1975 .

[3]  R. Lepping,et al.  Interplanetary magnetic field and magnetospheric substorms , 1977 .

[4]  J. Dungey Interplanetary Magnetic Field and the Auroral Zones , 1961 .

[5]  J. Burch Rate of erosion of dayside magnetic flux based on a quantitative study of the dependence of polar cusp latitude on the interplanetary magnetic field , 1973 .

[6]  C. C. Abston,et al.  Auroral electrojet magnetic activity indices AE (11) for 1972 , 1974 .

[7]  J. Burch Observations of interactions between interplanetary and geomagnetic fields , 1974 .

[8]  C. Kennel,et al.  Can the ionosphere regulate magnetospheric convection , 1973 .

[9]  Robert L. McPherron,et al.  The statistical magnetic signature of magnetospheric substorms , 1978 .

[10]  Harry E. Petschek,et al.  Magnetic Field Annihilation , 1963 .

[11]  P. Perreault,et al.  Reply [to “Comments on ‘A dusk‐dawn asymmetry in the response of the magnetosphere to the IMF Bz component’ by P. D. Perreault and Y. Kamide”] , 1978 .

[12]  B. Sonnerup,et al.  Magnetopause reconnection rate , 1974 .

[13]  P. Kintner,et al.  Correlated electric field and low-energy electron measurements in the low-altitude polar cusp. Progress report. [2000 km altitude] , 1976 .

[14]  J. Slavin,et al.  Magnetic flux transfer associated with expansions and contractions of the dayside magnetosphere , 1978 .

[15]  T. Pytte Comments on ‘A dusk‐dawn asymmetry in the response of the magnetosphere to the IMF Bz component’ by P. D. Perreault and Y. Kamide , 1978 .

[16]  Y. Kamide,et al.  A statistical study of the ‘instantaneous’ nightside auroral oval: The equatorward boundary of electron precipitation as observed by the Isis 1 and 2 satellites , 1977 .

[17]  Masahisa Sugiura,et al.  Auroral electrojet activity index AE and its universal time variations. , 1966 .

[18]  H. Garrett The role of fluctuations in the interplanetary magnetic field in determining the magnitude of substorm activity , 1974 .

[19]  G. Rostoker,et al.  Development of the polar electrojet during polar magnetic substorms , 1971 .

[20]  F. S. Johnson The driving force for magnetospheric convection , 1978 .

[21]  G. Siscoe,et al.  Aerodynamic aspects of the magnetospheric flow , 1964 .

[22]  V. Vasyliūnas Theoretical models of magnetic field line merging , 1975 .

[23]  S. Akasofu The roles of the north-south component of the interplanetary magnetic field on large-scale auroral dynamics observed by the DMSP satellite , 1975 .

[24]  K. Maezawa Magnetotail boundary motion associated with geomagnetic substorms , 1975 .