“…The early study by Choubey et al (2009) reported a bell-shaped transient anomaly, marked by the sharp negative-positive impulse, in association with an M 4.9 Kharsali earthquake of July 22, 2007. Later Choubey et al (2011), Arora et al (2012, and Kamra et al (2013) reported the season-dependant diurnal variations in radon, which were related with the saturation of the top soil layer and the temperature gradient in a borehole environment. There is growing evidence that emanation and transport of radon in the rock matrix is also affected by meteorological parameters like rainfall, soil moisture, pressure, temperature, both at transient and at seasonal time scales (Clements and Wilkening, 1974;Mogro-Campero and Fleischer, 1977;Ball et al, 1991;Pinault and Baubron, 1997;Muramatsu et al, 2002;Finkelstein et al, 2006;Adler and Perrier, 2009;Barbosa et al, 2010;Choubey et al, 2011;Gregorič et al, 2011;Zafrir et al, 2013).…”