Turbulent mixing from breaking oceanic internal waves drives a vertical transport of water,
heat and other climatically important tracers in the ocean, thereby playing an important role …

Numerical solutions of partial differential equations enable a broad range of scientific
research. The Dedalus project is a flexible, open-source, parallelized computational …

Oceanic flows are turbulent and multi-scale in nature, and are composed of fast internal
waves and slowly evolving balanced eddies. Contrary to conventional wisdom in physical …

Satellite observations of the last two decades have led to a major breakthrough emphasizing
the existence of a strongly energetic mesoscale turbulent eddy field in all the oceans. This …

The processes leading to the depletion of oceanic mesoscale kinetic energy (KE) and the
energization of near‐inertial internal waves are investigated using a suite of realistically …

The effects of internal waves (IWs), externally forced by high-frequency wind, on energy
pathways are studied in submesoscale-resolving numerical simulations of an idealized wind …

We study stimulated generation–the transfer of energy from balanced flows to existing
internal waves–using an asymptotic model that couples barotropic quasi-geostrophic flow …

An idealized storm scenario is examined in which a wind-generated inertial wave interacts
with a turbulent baroclinic quasigeostrophic flow. The flow is initialized by spinning up an …

Moored current observations in the northwestern South China Sea (SCS) captured two
events of near‐inertial waves (NIWs) induced by the tropical cyclones Conson and Mindulle …

Oceanic internal waves are a major driver for turbulent mixing in the ocean, which controls
the global overturning circulation and the oceanic heat and carbon transport. Internal waves …