The Antarctic Slope Front (ASF) is a strong gradient in water mass properties close to the
Antarctic margins, separating warm water from the Antarctic ice sheet. Heat transport across …

Accurate parameterizations of eddy fluxes across prograde, buoyant shelf and slope
currents are crucial to faithful predictions of the heat transfer and water mass transformations …

Most of the ocean's kinetic energy is contained within the mesoscale eddy field. Models that
do not resolve these eddies tend to parameterize their impacts such that the parameterized …

The transport of warm deep water (WDW) onto the Weddell Sea continental shelf is
associated with heat flux and strongly contributes to the melting of Antarctic ice shelves. The …

Abstract Eastern Boundary Upwelling Systems (EBUSs) host equatorward wind-driven near-
surface currents overlying poleward subsurface undercurrents. Various previous theories for …

Mesoscale eddies dominate the ocean kinetic energy reservoir. However, how and where
this energy flows out from the mesoscale remains uncertain. Here, a simplified mesoscale …

Oceanic mesoscale eddy mixing plays a crucial role in Earth's climate system by
redistributing heat, salt, and carbon. For many ocean and climate models, mesoscale eddies …

Isopycnal eddy mixing across continental slopes profoundly modulates the ocean circulation
and biogeochemistry. Yet this process must be parameterized in coarse‐resolution ocean …

Mesoscale eddy buoyancy fluxes across continental slopes profoundly modulate the
boundary current dynamics and shelf–ocean exchanges but have yet to be appropriately …

Ocean general circulation models at the eddy-permitting regime are known to under-resolve
the mesoscale eddy activity and associated eddy-mean interaction. Under-resolving the …