Using the Indian MST Radar Noise-Level Observations of Stratosphere-Troposphere Replace were made over the tropical station Gadanki

The mesosphere stratosphere-troposphere radar at Gadanki was used to record the climates of stratosphere disturbance into the tropospheric through the Indian Summer Monsoon. The existence of an enhanced signal-to-noise ratio of 3 dB and measurement powers complete supernatural size of greater than 0.2 ms
^-1
in the locality of the troposphere through the Indian Summer Monsoon is the most important and novel observation. From April to June, downdrafts (updrafts) predominate near the tropopause (July to March). The ten years of ozone dimensions from the five years of in-situ ozonesonde explanation also support the outcome of stratosphere air intrusion. A thorough analysis reveals that the tropical easterly jet's turbulence near the tropopause, horizontal advection, and troposphere height changeability is the leading candidate for ozone ship from the stratospheric to the tropospheric. In contrast, during the ISM, the tropical troposphere heat has an important impact on the carrying of water steam from the tropopause to the stratopause. The idea of the present revision is to use Indian MST radar to qualitatively construct the climate of these replace processes over Gadanki.