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High resolution (150 m) wind measurements from 13–17July 2004 by Mesosphere-Stratosphere-Troposphere (MST) radar and 15–16July 2004 by Lower Atmospheric Wind Profiler (LAWP) have been used to studythe time variation of turbulence intensity. Layers of higher turbulence areobserved in the lower stratosphere on 15–16 July which give rise to mixingin the region. Enhancement in short-period gravity wave activity andturbulent layers are observed after 22:00 LT which could be due to a dryconvection event that occurred at that time. The breakdown of theconvectively generated high frequency waves seems to have given rise to theturbulence layers. Wind shear is found to be high above the easterly jet,but very poor correlation is observed between square of wind shear andturbulence parameters in the region. The heights of the turbulent layers inthe lower stratosphere do not correlate with levels of minimum Richardsonnumber. A monochromatic inertia gravity wave could be identified during13–17 July 2004. A non-linear interaction between the waves of differentscales as proposed by Hines (1992) might also be responsible for thebreakdown and generation of turbulence layers

High resolution observations of turbulence in the troposphere and lower stratosphere over Gadanki