Since the discovery of the Earth's Van Allen radiation belts over 50 years ago (Van Allen & Frank, 1959), determining the physical processes responsible for their dynamics have been a major focus of space physics research (e.g., Friedel et al., 2002). The dynamics of the trapped relativistic electron population with energies from hundreds of kilo electronvolts (∼100 keV) to millions of electronvolts (∼1 MeV) during geomagnetic storms is of particular interest because of their potential impact on satellite electronics through deep-dielectric charging (Baker et al., 1994). Electrons can be lost at the beginning of the storm before the subsequent acceleration of a source population to MeV energies, which can partially or completely replace those which are lost, in some cases creating radiation orders of magnitude stronger than that which existed pre-storm (e.g., Reeves et al., 2003). In particular, interaction with high-frequency plasma waves, such as chorus (e.g., Lee et al., 2013;Shprits et al., 2007), electromagnetic ion cyclotron (EMIC) (e.g., Ukhorskiy et al., 2010;Usanova et al., 2014), or plasmaspheric hiss (e.g., Thorne et al., 1973) waves, can cause loss into the atmosphere. Meanwhile, ultra-low frequency (ULF) plasma waves (Mann et al., 2016) can cause particles to be transported outwards to the last closed drift shell (LCDS) and lost at the magnetopause into the solar wind in a process known as magnetopause shadowing (e.g., Olifer et al., 2018;Turner et al., 2012). The relative importance of these processes continues to be hotly debated (Mann et al., 2018;Shprits et al., 2018). This paper, in particular, focuses on investigating whether the LCDS dynamics can explain the fast magnetopause shadowing losses.Recent studies have shown that a compression of the outer magnetospheric boundary can cause intense electron radiation belt losses occurring on very short ( 𝐴𝐴 𝐴 1 day) timescales. For example, Olifer et al. ( 2018) showed that the LCDS location of the Van Allen belt electrons and its dynamics can explain rapid and intense dropouts of relativistic electrons in some of the most intense geomagnetic storms of the last decade. It is also interesting to investigate on a statistical basis whether a substantial compression of the magnetopause, characterized by inward motion of the LCDS, can cause a radiation belt dropout in every storm and