A total of nine stratospheric warming events are identified out of 12 winters using GPSRO measurements.
This paper to describe the SSW impact on pauses using satellite and reanalysis datasets.
The altitude of tropopause is observed to have decreased by ~ 0.7 km during SSW events.
The increase in potential vorticity transport is higher in high latitudes in the middle and the near equator.
The gravity wave energy values are all most 4 times observed during the SSW events.