The universal time variation of geomagnetic activity
C. T. Russell
Abstract
C. T. Russell
Abstract
Geomagnetic activity exhibits both annual and daily variations. We examine these variations in the Am index which was designed to provide an accurate measure of the Universal Time variation of geomagnetic activity. The dayside reconnection process can quantitatively account for the observed variation in both indices. Control of these variations by the angle of the flow relative to the dipole axis is weaker than control by reconnection.
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Geomagnetic activity exhibits both annual and daily variations. We examine these variations in the Am index which was designed to provide an accurate measure of the Universal Time variation of geomagnetic activity. The dayside reconnection process can quantitatively account for the observed variation in both indices. Control of these variations by the angle of the flow relative to the dipole axis is weaker than control by reconnection.
Key concepts: Earth's magnetic field, Universal Time, Variation (astronomy), Geomagnetic secular variation, Physics, Local time, Atmospheric sciences, Geophysics