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- W2912077563 abstract "Abstract Freshwater transports ( F ov ) by the Atlantic meridional overturning circulation (AMOC) are sensitive to salinity distributions and may determine AMOC stability. However, climate models show large salinity biases, distorting the relation between F ov and the AMOC. Using free‐running models and ocean reanalyses with realistic salinities but quite different AMOCs, we show that the fresh Antarctic Intermediate Water layer eliminates salinity differences across the AMOC branches at ~1,200 m, ∆ S 1200 m , which decouples F ov from the AMOC south of ~10°N. As the Antarctic Intermediate Water disappears north of ~10°N, a large ∆ S 1200 m allows the AMOC to drive substantial southward F ov in the North Atlantic. In the South Atlantic the 0–300 m zonal salinity contrasts control the gyre freshwater transports F gyre , which also determine the total freshwater transports. This decoupling makes the southern F ov unlikely to play any role in AMOC stability, leaving indirect F gyre feedbacks or F ov in the north, as more relevant factors." @default.
- W2912077563 created "2019-02-21" @default.
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- W2912077563 date "2019-02-25" @default.
- W2912077563 modified "2023-10-12" @default.
- W2912077563 title "Decoupled Freshwater Transport and Meridional Overturning in the South Atlantic" @default.
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- W2912077563 doi "https://doi.org/10.1029/2018gl081328" @default.
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