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HF radar observations of high‐velocity E region echoes from the eastward auroral electrojet
Author(s) -
Makarevich Roman A.
Publication year - 2008
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2008ja013204
Subject(s) - electrojet , geology , radar , physics , equator , doppler effect , geophysics , geodesy , latitude , magnetic field , earth's magnetic field , astronomy , telecommunications , quantum mechanics , computer science
We present a statistical analysis of short‐range E region echoes observed by the Super Dual Auroral Radar Network (SuperDARN) HF radars in the evening sector (16–22 MLT) over 3 years. Significant populations of the high‐velocity (350–450 m/s) E region echoes similar to the classical Type 1 echoes are observed by 4 zonally‐looking SuperDARN radars at small magnetic L ‐shell angles. The spatial occurrence pattern of Type 1 echoes is investigated. It is shown that the latitudinal (slant range) extent of the region where Type 1 echoes occur increases as the L ‐shell angle decreases, which is interpreted as widening of the aspect angle instability cone with the flow angle decrease. The echoes with unusually high velocities (500–600 m/s) observed by the Syowa East HF radar are also investigated. These echoes are seen at all L ‐shell angles (15°–75°) and their Doppler velocity increases with range and exhibits little variation with L ‐shell angle. The echoes occur at ranges 360–495 km when the strong low‐velocity echoes ( P > 30 dB, V < 200 m/s) are observed at ranges 225–360 km. We analyze the echo occurrence and velocity dependencies on the simultaneously observed F region echo velocity (plasma drift velocity) and E region echo power. It is suggested that the auroral E region echoes with unusually high velocities observed at large flow angles are similar to the vertically propagating Type 1 echoes reported previously in observations at the magnetic equator and are likely to be secondary waves generated through nonlinear mode coupling processes.

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