High-latitude dayside electric fields and currents during strong northward interplanetary magnetic field - Observations and model simulation

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Interplanetary Magnetic Fields, Ionospheric Currents, Space Plasmas, Earth Magnetosphere, Ion Motion, Magnetometers, Radar Data, Solar Wind

Scientific paper

On July 23, 1983 the IMF turned strongly northward, becoming about 22 nT for several hours. Using a combined data set of ionospheric convection measurements made by the Sondre Stromfjord incoherent scatter radar and convection inferred from Greenland magnetometer measurements, the onset of the reconfiguration of the high-latitude ionospheric currents is found to occur about 3 min after the northward IMF encounters the magnetopause. The large-scale reconfiguration of currents, however, appears to evolve over a period of about 22 min. These observations and the results of numerical simulations indicate that the dayside polar-cap electric field observed during strong northward IMF is produced by a direct electrical current coupling with the solar wind.

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