Magnetospheric perturbations driven by the solar wind cause substantial fluctuations of outer belt electron fluxes over short timescales. Such events are called dropouts. During these depletion events, the electron flux > 0.1 MeV can drop by several orders of magnitude in less than a few hours, often during geomagnetic storms (Turner et al., 2012). Reeves et al. (2003) performed a pioneering study of the variations of 1.8-3.5 MeV electron fluxes to geomagnetic storms from 1989 through 2000. They found that 53% of the storms caused an enhancement of the fluxes of electrons at geosynchronous orbit in comparison to the prestorm flux, 19% caused a decrease in fluxes, while 28% resulted in no significant change of fluxes. Benck et al. (2013) also analyzed statistically electron flux observations from DEMETER and SAC-C at Low Earth Orbit (LEO) during quiet and disturbed periods and developed a transient observation-based particle (TOP) model. Many storms were later studied with Van Allen Probes launched in September 2012 (cf. review of Ripoll et al., 2020 and more specifically, the introduction of Turner et al., 2019 for a review on studies dedicated to storms). Turner et al. (2019) made a very complete analysis of the flux evolution during 110 storms that occurred between September 2012 and September 2017. It complemented the study of Turner et al. (2015) in which the authors had analyzed 52 storms from September 2012 to February 2015. For 1.5 MeV electrons at L = 6, they found 39% of the storms resulted in an enhancement, 26% resulted in depletion, and 35% resulted in no significant change in relative levels of the prestorm and post storm electron fluxes. They also reported that MeV electrons had the highest occurrence of dropout mainly at L > 4. Moya et al. (2017) considered 78 storms between September 2012 and June 2016. They observed that more intense storms caused the radiation belt to move inward toward the Earth.