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- W2025697726 abstract "Abstract A dual coherent 50 MHz auroral radar installed at Siple Station, Antarctica, continuously monitored echo intensity and mean-Doppler velocity from 29 December 1976 until late March 1978. We describe here the experimental technique and present some statistical results including yearly averaged echooccurrence patterns and irregularity drift velocity characteristics. Our results show that: 1. (1) the irregularity drifts are approximately westward (poleward electric fields) in the evening, and eastward (equatorward electric fields) in the morning following the electric field reversal in the region of the Harang discontinuity; 2. (2) the Harang discontinuity under disturbed conditions (average K p = 5 0 ) as seen by both radars is located around 2100–2300 MLT; 3. (3) the relationship between the irregularity drift velocity and the actual electron drift velocity is strongly dependent on the angle between the radar beam and the earth's magnetic field, as predicted by linear theory." @default.
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- W2025697726 date "1982-06-01" @default.
- W2025697726 modified "2023-09-27" @default.
- W2025697726 title "Auroral radar observations at Siple Station, Antarctica" @default.
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- W2025697726 doi "https://doi.org/10.1016/0021-9169(82)90142-8" @default.
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