Abstract:<p><span>The upper limb of the Atlantic Meridional Overturning Circulation (AMOC) brings shallow interocean contributions to replenish the North Atlantic export of deepwaters. It is primarily formed in the southern South Atlantic where the converging entrainment of Pacific and Indian Ocean waters meet and incorporate into the South Atlantic subtropical gyre (SASG). Here, the human-induced response of AMOC and SASG near-surface pathways is illustrated according to CESM1 Large Ensembl… Show more
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