“…Therefore, while performing the Earth's surface deformation observations, the same network of GPS receivers can also be used simultaneously and continuously to monitor the ionospheric TEC (Sardon et al 1994, Leick 1995, Liu et al 1996. Recently, an apparent reduction in GPS TEC was observed a few days prior to some strong earthquakes (Calais and Minster 1995, Liu et al 2001, Zhou et al 2009, Xia et al 2010. Devi et al (2008) reported that the manifestation of seismo-ionospheric effects should be strongly dependent (among others) on regional features of the ionosphere and such an increase in TEC is seen when the epicentre lies away from the observing stations (latitude, longitude or both).…”