The ocean circulation is a cause and consequence of fluid scale interactions ranging from
millimeters to more than 10,000 km. Although the wind field produces a large energy input to …

We review the physics of near-inertial waves (NIWs) in the ocean and the observations,
theory, and models that have provided our present knowledge. NIWs appear nearly …

This study provides an overview of the coupled high‐resolution Version 1 of the Energy
Exascale Earth System Model (E3SMv1) and documents the characteristics of a 50‐year …

Internal tides power much of the observed small-scale turbulence in the ocean interior. To
represent mixing induced by this turbulence in ocean climate models, the cascade of …

Oceanic mesoscale structures such as eddies and fronts can alter the propagation, breaking
and subsequent turbulent mixing of wind-generated internal waves. However, it has been …

The distribution of wind‐induced internal wave energy in the world's oceans is investigated
using a full three‐dimensional primitive equation model. Special attention is directed to the …

The currently available theoretical and observational evidence for a latitudinal structure of
thermocline vertical diffusivity is synthesized and included in a state of the art coupled …

Wind-induced near-inertial energy has been believed to be an important source for
generating the ocean mixing required to maintain the global meridional overturning …

The propagation characteristics of near‐inertial waves (NIWs) and how mesoscale and
submesoscale processes affect the waves' vertical penetration are investigated using …

An Energy Compartment Model for Propagation, Nonlinear Interaction, and Dissipation of
Internal Gravity Waves in: Journal of Physical Oceanography Volume 44 Issue 8 (2014) …