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Reasons from basin-scale budgets, three-dimensional circulation, and forcing-transport-transformation coupling through θ–S and OMP water-mass analysis, transient-tracer ventilation ages (CFC/SF₆/¹⁴C), GO-SHIP/Argo/SOCAT networks, and TEOS-10 thermodynamics while treating mesoscale aliasing of single sections, mixed real-time and delayed-mode QC, and freshwater-driven salinity confounds as first-class failure modes.