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E- and F-region coupling between an intense sporadic E layer and a mesoscale traveling ionospheric disturbance

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Figure

Fig. 1. Electron density through the disturbed night of 20–21 Febru-ary 1999 with the azimuth position shown by the black triangularline
Fig. 3. Shown is a time sequence of sequential back-and-forth azimuth scan cones of the Arecibo electron density measurements from 55 kmto 500 km together with the beams of the CUPRI and Illinois radars to 100 km altitude and the intersecting magnetic field
Fig. 4. Velocity components using the Sulzer et al. (2005). regular-ization at a height of 367 km.
Fig. 5. E-region (light solid line), F-region (heavy solid line), andvalley-region (dashed line) Pedersen conductivities.
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