E-region bifurcation and magnetic field related Bragg backscattered spectral events observed at high-latitude by MF radar

We report on novel spectral characteristics of E‐region backscatter acquired using a 1.94 MHz Medium Frequency (MF) radar above the high‐latitude Antarctic station Davis (68.6°S). Two distinctive Doppler spectra are observed: one that exhibits bifurcation in Doppler velocity (or frequency) with one, or occasionally more, near symmetrical spectral side‐bands (here labelled SSE); and a second that exhibits broad‐band spectra related to the magnetic field topology (here labelled FRE). Both spectral forms reveal a characteristic quasi‐hyperbolic spectral form that diverges in Doppler velocity with range. We discuss the properties of these two spectral forms including: Doppler spectral shape; power spectra; angle‐of‐arrival (AOA) of backscattered sources; and their diurnal and day‐to‐day occurrence distributions for our campaign interval. Interestingly, the E‐region SSE observed at a height near 100 km were observed coincidentally with D‐region polar mesosphere summer echoes (PMSE) in the height range 82–92 km, when colocated data were available.