These two papers indicate that in the last decade or so, formation of highly saline cold deep water formation around the margin of Antarctica has increased and strengthened. In the long term more cold deep water supply from Antarctica will result in a cooling effect on global climate. Antarctica is the biggest global source of cold saline bottom water which drives the Thermo Haline Circulation.
Antarctic bottom water (AABW) is one of the major deep water compartments of the global oceans. In the last half century or so the supply of AABW from its source in Antarctica had been observed to decline; however Alessandro Salvini et al 2020 reported in Nature Geosciences that this decline has reversed. Now the supply of AABW from the Ross Sea is increasing:
The same observation was made in the Weddell Sea by Kerr et al. 2018. In that Antarctic Sea the supply of bottom water (Weddell Sea Bottom Water, WSBW) also turned around from decline to increase, around 2005:
Thus several lines of evidence point to strengthening supply of deep cold water from Antarctica, to the global ocean circulation. Which might put a crimp in global warming – eventually.