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The team of Du Yan, a researcher at the State Key Laboratory of Tropical Marine Environment, South China Sea Institute of Oceanology, Chinese Academy of Sciences, teamed up with Xie Shangping , a professor at the SCRIPPS Institute of Oceanography in the United States , and scientists at Ocean University of China
Sub-Antarctic Mode Water ( SAMW ) is a water mass with vertical uniformity formed between the sub-Antarctic front and the subtropical front in the Southern Ocean, which is strongly mixed in winter.
This study analyzed the changes in the sub-Antarctic modal water from 1901 to 2300 in the historical experiment historical and the future scenario RCP4.
Studies have shown that the change of SAMW mainly depends on the evolution of sea surface buoyancy flux, while the westerly zone has little influence due to the polar movement
This study gave the first time the speed of SAMW to global warming, and proposed that the volume of SAMW will not increase under the background of stronger westerly winds in the future
Related paper information: https://link.
Figure 1.
