“…Further, TEC at 1930 LT, at any location within the equatorial ionization anomaly (EIA) zone, decides the maximum amplitude of the scintillations, namely, the S 4max [ Bagiya et al , ]. The strength of the EIA represented by the crest‐to‐trough ratio has been used as a parameter to provide clues to the favorable/unfavorable conditions for the initiation of the instability [ Raghavarao et al , ; Alex et al , ; Sridharan et al , , ; Valladares et al , ; Thampi et al , , ]. As far as the neutral dynamical parameters controlling the instability are concerned, the vertical winds are known to be capable of tilting the balance [ Sekar and Raghavarao , ; Sridharan et al , , and references therein].…”