The recent Kwajalein radar backscatter observations of 11‐cm irregularities at high altitudes (∼500 km) during equatorial spread F are explained in terms of the kinetic lower‐hybrid‐drift instability. The absence of radar backscatter from 11‐cm irregularities at lower altitudes (∼240 km) is attributed to the stabilizing influence of electron‐neutral collisions.
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Huba et al. (1981) studied this question.
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