Turbulent isopycnal mixing dominates thermohaline transformations of intermediate ocean waters.

ABSTRACT: The ocean, because of its ability to store heat and as the biggest mediator of water exchanges on Earth, modulates the climate from years to centuries. By combining Water Mass transformation and the Temporal-Residual-Mean frameworks, together with a direct estimation of turbulent diffusivity (computed through an artificial intelligence method), we determine temperature and salinity transformations along density surfaces. Because isopycnal transformations barely alter the density field, they remain hidden from the ocean dynamics. Here we unveil these hidden, isopycnal transformations from in situ observations at 1000-m depth. We shows that these isopycnal transformations are 5 times as large as their diapycnal counterpart and are occurring for  ~ 67% in the Southern Ocean. Our estimations s

SUBMITTER: Sevellec F 

PROVIDER: S-EPMC12594881 | biostudies-literature | 2025 Nov

REPOSITORIES: biostudies-literature