We present a new, simple and physically motivated parameterization, based on the ratio of
Thorpe and Ozmidov scales, for the irreversible turbulent flux coefficient. Importantly …

Abstract The Southern Ocean (SO) connects major ocean basins and hosts large air‐sea
carbon fluxes due to the resurfacing of deep nutrient and carbon‐rich waters. While wind …

Ocean turbulent mixing is a key process affecting the uptake and redistribution of heat,
carbon, nutrients, oxygen and other dissolved gasses. Vertical turbulent diffusivity sets the …

The turbulent ocean surface boundary layer is a key part of the climate system affecting both
the energy and carbon cycles. Accurately simulating the boundary layer is critical in …

Characterizing how ocean turbulence transports heat is critically important for accurately
parameterizing global circulation models. We present a novel data‐driven approach for …

Understanding how turbulence enhances irreversible scalar mixing in density-stratified
fluids is a central problem in geophysical fluid dynamics. While isotropic overturning regions …

Submarine canyons that incise continental slopes are considered an important conduit for
transport of suspended matter between shelf seas and deep-ocean. However, the exact …

Seismic reflection profiling of thermohaline structure has the potential to transform our
understanding of oceanic mixing and circulation. This profiling, which is known as seismic …

Turbulent mixing at the sub‐meter scale is an essential component of the ocean's meridional
overturning circulation and its associated global redistribution of heat, carbon, nutrients …

Abstract In the Arctic Ocean, vertical transport of heat by turbulent mixing is ultimately
coupled to the sea‐ice cover, with immediate and far‐reaching impacts on the climate and …