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Effects of high latitude atmospheric gravity wave disturbances on artificial HF radar backscatter

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Figure

Fig. 1. Map of the instruments used and their fields-of-view. Thesquare denotes the CUTLASS Hankasalmi radar
Fig. 2. Top panel: range-time-intensity (RTI) plot of CUTLASS radar backscatter signal-to-noise ratio (SNR) at 13.2 MHz
Fig. 3. Elevation angle measurements from the CUTLASS HF radar. Top panel: 13.2 MHz; centre panel: 15.1 MHz; bottom panel:18.0 MHz
Fig. 4. Simulation of how the region where the HF pump reachesthe upper-hybrid resonance altitude varies as the TID “E” passesover the transmitter location
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