The plasmasphere is the innermost region of the Earth's magnetosphere, which is filled with cold (low energy ∼1-10 electron volt (eV) and dense (10-10 4 cm −3)) plasma of ionospheric origin trapped to the Earth's magnetic field, forming a thermal plasma cloud encircling the Earth (Darrouzet et al., 2009b; Lemaire et al., 1998). Outside the plasmasphere, the plasma characteristics change abruptly to tenuous (1 cm −3), hot (high energy ∼100 eV) plasma. The boundary that separates this outer region of the highly energized, low-density plasma from the plasmasphere, is called plasmapause. The plasma motions in the inner magnetosphere are dominated by large scale electric fields. The corotation electric field enforces the corotation of cold plasma near the Earth, and the magnetospheric convection electric field (generated by the interaction between the solar wind and the magnetosphere) causes the loss of cold plasma outside the plasmasphere. The convection electric field, being a key factor for the formation of the plasmapause (Pierrard et al., 2008), the location and sharpness of the plasmapause vary with