Using the in situ measurements of ROCSAT‐1 satellite during 181 geomagnetic storms happened from July 1999 to June 2004, a superposed epoch analysis of the equatorial plasma depletions (EPDs) occurrence is conducted. At postsunset hours (1800–2200 LT), the EPDs occurrence is enhanced shortly at the storm onset, but afterward, a long‐last suppression dominates. The EPDs occurrence at Midnight (2200–0200 LT) generally shares a similar pattern to that at postsunset hours. The occurrence at predawn (0200–0400) gradual increases near storm onset and reach its maximum at 6–9 hr and decays until 18 hr. For a given longitude at postsunset/midnight, the EPDs occurrence tends to be suppressed or promoted when the EPDs do or do not prevail. The disturbed vertical plasma drift generally determines the inhibition/promotion of the EPDs occurrence at postsunset/predawn. However, for predawn EPDs occurrence, the plasma vertical drift cannot well explain the longitudinal variation. The continuous observations from consecutive orbits of ROCSAT‐1 are carefully compared and the result suggests that the geomagnetic storm‐induced additional predawn EPDs are preferred to be the longer‐lived developed EPDs rather than fresh EPDs. In addition, a possible mechanism concerning the background plasma density enhancement which might be related with the energetic electrons induced nighttime ionization is proposed.