Depth‐averaged eddy buoyancy diffusivities across continental shelves and slopes are
investigated using a suite of eddy‐resolving, process‐oriented simulations of prograde …

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 …

A physically plausible lower bound on the spatially varying geostrophic mesoscale eddy
energy dissipation time‐scale within the ocean, related to the geographical energy transfer …

The global ocean overturning circulation, critically dependent on the global density
stratification, plays a central role in regulating climate evolution. While it is well known that …

The velocity perturbations and Reynolds stresses associated with finite-amplitude Holmboe
instabilities are investigated using linear stability analysis, numerical simulations, and …

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 …

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

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 Ocean components of Earth System Models employed for climate projections do not
routinely resolve mesoscale eddies for computational cost reasons, and the associated …

Mesoscale eddy prediction has been a big challenge to oceanographers and marine
environment forecasters. Although the traditional initialization for the prediction, ie, through …