Magnetic disturbance effects in the E region of the ionosphere

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Atmospheric Circulation, Critical Frequencies, E Region, Ionospheric Disturbances, Magnetic Disturbances, Daytime, Electric Current, Magnetic Field Configurations, Midlatitude Atmosphere, Thermosphere

Scientific paper

Detailed studies of the daytime E-region critical frequency at Aberystwyth (geomagnetic latitude +56 deg) show clear evidence for changes associated with both the axisymmetric (Dst) and asymmetric (DS) components of the disturbance magnetic field. Comparison of the sensitivity of the E-region peak density with these two influences shows that the changes cannot entirely (if at all) be ascribed to the influence of electric currents in the region. It is suggested that a major role is played by dynamical influences associated with the neutral-air 'storm circulation' which distributes the energy fed into the auroral region to lower latitudes.

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