Quantification of high latitude electric field variability

Physics

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Atmospheric Composition And Structure: Thermosphere-Energy Deposition, Ionosphere: Electric Fields, Ionosphere: Plasma Convection, Magnetospheric Physics: Plasma Convection

Scientific paper

Variability in the high latitude electric field has been identified as a major contributor to global Joule heating. Electric field patterns from the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) procedure are used to characterize the E-field temporal variability over the course of 18 hours. The standard deviation of the E-field magnitude on May 4, 1998 often exceeds the average value of the E-field magnitude. A significant fraction of this variability arises from oscillations with period less than one hour. This confirms that Joule heating calculations based on time-averaged E-fields may significantly under-predict the heating.

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