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 …

For several decades, jets and fronts have been known from observations to be significant
sources of internal gravity waves in the atmosphere. Motivations to investigate these waves …

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 …

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 …

Group speed of mode-1 M 2 internal tide over the entire world. Representative rays
emanating from known generation sites are also plotted in black. Circles indicate the daily …

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 “near-inertial” part of the internal wave continuum is dominant and also different from
the rest of the spectrum. A simple possible reason for the difference is that waves generated …

Annual Cycle and Depth Penetration of Wind-Generated Near-Inertial Internal Waves at Ocean
Station Papa in the Northeast Pacific in: Journal of Physical Oceanography Volume 42 Issue 6 …

Stimulated Imbalance and the Enhancement of Eddy Kinetic Energy Dissipation by Internal
Waves in: Journal of Physical Oceanography Volume 47 Issue 1 (2017) Jump to Content …