A lidar system has been used at Gadanki (13.5 degrees, 79.2 degreesE) to st
udy the characteristics of aerosol layer (cloud) occurring just below the t
ropical tropopause, The preliminary results of the lidar observations indic
ate that the cloud occurs similar to 2 km below the tropopause. The top and
bottom edges of the cloud have propensity for ice crystal presence with li
quid droplets/vapours in-between. The clouds show temporal fluctuations tin
their backscattering ratio) with temporal scales of the order of 30-90 min
.