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Global distribution of ionospheric and field‐aligned currents during substorms as determined from six IMS meridian chains of magnetometers: Initial results

1982; American Geophysical Union; Volume: 87; Issue: A10 Linguagem: Inglês

10.1029/ja087ia10p08228

2156-2202

Y. Kamide, B.‐H. Ahn, S.‐I. Akasofu, W. Baumjohann, E. Friis‐Christensen, H. W. Kroehl, H. Maurer, A. D. Richmond, G. Rostoker, R. W. Spiro, J. K. Walker, Alexander Zaitzev,

Earthquake Detection and Analysis

As a part of the joint efforts of operating six meridian chains of magnetometers during the IMS, magnetic records from 70 stations are used to deduce patterns of electric fields and currents in high latitudes on March 17, 18, and 19, 1978. First of all this data set is used to examine the fidelity of the AE (12) index by comparing it with the AE (70) index and also the fidelity of the AL (70) index as a measure of the total westward electrojet intensity. The coefficients for the two correlations are found to be more than 0.8. Then the distribution of both ionospheric currents and field‐aligned currents, as well as the electric field, are for the first time determined with a time resolution of 5 min by using an appropriate conductivity distribution model. Although much improvement is still needed for better accuracy, especially in the estimation of ionospheric conductivity, it has now become possible to study the growth and decay of the three‐dimensional current system over the north polar region during individual magnetospheric substorms with sufficient time resolution. Our initial results show that the gross features of the instantaneous distributions of the ionospheric and field‐aligned currents are remarkably similar to the daily average pattern during a very weak activity and at different substorm epochs and that the large‐scale current pattern grows and decays systematically as a whole. There are, however, significant changes in local scales.