192-198The MST radar observations
at Gadanki, Tirupati (13.5°N, 79.2°E), during 1995-96 winter showed an anomalous
wind pattern in the troposphere and lower stratosphere. During the season the
mean zonal wind between 3.6 km and 21 km region was westerly and the vertical velocity
was downward. The zonal wind exhibited a change from the normal pattern of
winter westerlies into easterlies in the troposphere and lower stratosphere during
January 1996. The radar data combined with radiosonde and National Centers for Environmental
Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data
showed that the anomalous features are associated with the north-south movement
of anticyclones during the passage of western disturbances over north-west India.
Such process of a midlatitude-tropics interaction is further evidenced as intrusion
of the upper air trough from the midlatitudes into the tropics