Stratospheric Circulation in the Southern Hemisphere: Links to Tropical Winds, Ozone and the Hunga Eruption—Part II: Evidence From a Global Chemistry‐Climate Model
The Southern Hemisphere (SH) stratospheric circulation can be categorized based upon the development of a Low‐Latitude Jet (LLJ) in the upper stratosphere during winter months. We analyze the dynamics of the LLJ based on a large ensemble of chemistry‐climate model simulations, supported by reanalysis data. The LLJ is...