Oceanic vertical mixing: A review and a model with a nonlocal boundary layer parameterization

WG Large, JC McWilliams, SC Doney - Reviews of geophysics, 1994 - Wiley Online Library
If model parameterizations of unresolved physics, such as the variety of upper ocean mixing
processes, are to hold over the large range of time and space scales of importance to …

Dynamics of winds and currents coupled to surface waves

PP Sullivan, JC McWilliams - Annual Review of Fluid Mechanics, 2010 - annualreviews.org
We discuss the coupling processes between surface gravity waves and adjacent winds and
currents in turbulent boundary layers. These processes mediate exchanges of momentum …

[HTML][HTML] Climate process team on internal wave–driven ocean mixing

JA MacKinnon, Z Zhao, CB Whalen… - Bulletin of the …, 2017 - journals.ametsoc.org
Climate Process Team on Internal Wave–Driven Ocean Mixing in: Bulletin of the American
Meteorological Society Volume 98 Issue 11 (2017) Jump to Content Jump to Main Navigation …

[HTML][HTML] Global patterns of diapycnal mixing from measurements of the turbulent dissipation rate

AF Waterhouse, JA MacKinnon… - Journal of Physical …, 2014 - journals.ametsoc.org
Global Patterns of Diapycnal Mixing from Measurements of the Turbulent Dissipation Rate in:
Journal of Physical Oceanography Volume 44 Issue 7 (2014) Jump to Content Jump to Main …

A global perspective on Langmuir turbulence in the ocean surface boundary layer

SE Belcher, ALM Grant, KE Hanley… - Geophysical …, 2012 - Wiley Online Library
The turbulent mixing in thin ocean surface boundary layers (OSBL), which occupy the upper
100 m or so of the ocean, control the exchange of heat and trace gases between the …

[HTML][HTML] UK Global Ocean GO6 and GO7: A traceable hierarchy of model resolutions

D Storkey, AT Blaker, P Mathiot… - Geoscientific Model …, 2018 - gmd.copernicus.org
Versions 6 and 7 of the UK Global Ocean configuration (known as GO6 and GO7) will form
the ocean components of the Met Office GC3. 1 coupled model and UKESM1 earth system …

[HTML][HTML] Upper-ocean inertial currents forced by a strong storm. Part I: Data and comparisons with linear theory

EA D'Asaro, CC Eriksen, MD Levine… - Journal of Physical …, 1995 - journals.ametsoc.org
A strong, isolated October storm generated 0.35–0.7 ms− 1 inertia] frequency currents in the
40-m deep mixed layer of a 300 km× 300 km region of the northeast Pacific Ocean. The …

The impact of oceanic near-inertial waves on climate

M Jochum, BP Briegleb, G Danabasoglu… - Journal of …, 2013 - journals.ametsoc.org
Abstract The Community Climate System Model, version 4 (CCSM4) is used to assess the
climate impact of wind-generated near-inertial waves (NIWs). Even with high-frequency …

A new coupled, one-dimensional biological-physical model for the upper ocean: Applications to the JGOFS Bermuda Atlantic Time-series Study (BATS) site

SC Doney, DM Glover, RG Najjar - Deep Sea Research Part II: Topical …, 1996 - Elsevier
This paper presents a new coupled, one dimensional biological-physical model applied to
the subtropical region near Bermuda. The physical component of the model, which is driven …

Model‐predicted distribution of wind‐induced internal wave energy in the world's oceans

N Furuichi, T Hibiya, Y Niwa - Journal of Geophysical …, 2008 - Wiley Online Library
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 …