In this paper we present the characteristics of mid‐latitude irregularities first observed with the 52 MHz Chung‐Li radar. Intense type‐1 echoes with Doppler velocities of about 270 m/s (slightly smaller than the nominal ion‐acoustic wave speed of 360 m/s) in the height range from 103.1 km to 104.5 km lasted for about 2 minutes. The range‐time variations of sequential power spectra indicate that the patch of type‐1 irregularities moved toward the radar at a rate of about 42 m/s. The zonal drift motions of the type‐1 and type‐2 irregularities obtained from an interferometry technique showed that the irregularities drifted eastward with an average speed of 84 m/s.
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Huang et al. (1998) studied this question.
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