“…The important aspects of these studies include: propagation characteristics of gravity waves in the realistic atmosphere (Midgley and Liemohn, 1966;Hines and Reddy, 1967;Lindzen, 1970), wave-mean flow interactions (Booker and Bretherton, 1967;Lindzen, 1973;Dunkerton, 1980;McIntyre, 1980), generation of turbulence and enhanced diffusion (Weinstock, 1976;Lindzen, 1981) and wave saturation and its effects (Fritts, 1984;Fritts and Rastogi, 1985). In recent years, the Rayleigh lidar technique has emerged as an effective means to study the gravity wave activity in the middle atmosphere over the height range of 30-70 km Hauchecorne, 1981, 1991;Wilson et al, 1990a, b;Gardner et al, 1989;Whiteway and Carswell, 1995;McDonald et al, 1998;Sivakumar et al, 2006;Ramkumar et al, 2006;Antonita et al, 2007).…”