During its periodic motion, a particle floating at the free surface of a water wave experiences a net drift velocity in the direction of wave propagation, known as the Stokes drift (Stokes …
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 …
In the long term development of the research on wind waves and their modelling, in particular of the inner and coastal seas, the present situation is framed with a short look at …
A signature of submesoscale flows in the upper ocean is skewness in the distribution of relative vorticity. Expected to result for high Rossby number flows, such skewness has …
Ø Breivik, K Mogensen, JR Bidlot… - Journal of …, 2015 - Wiley Online Library
The NEMO general circulation ocean model is extended to incorporate three physical processes related to ocean surface waves, namely the surface stress (modified by growth …
Q Li, BG Reichl, B Fox‐Kemper… - Journal of Advances …, 2019 - Wiley Online Library
Six recent Langmuir turbulence parameterization schemes and five traditional schemes are implemented in a common single‐column modeling framework and consistently compared …
Large eddy simulations of the Craik‐Leibovich equations are used to assess the effect of misaligned Stokes drift and wind direction on Langmuir cells in the ocean mixed layer …
N Suzuki, B Fox‐Kemper - Journal of Geophysical Research …, 2016 - Wiley Online Library
The wave‐averaged, or Craik‐Leibovich, equations describe the dynamics of upper ocean flow interacting with nonbreaking, not steep, surface gravity waves. This paper formulates …
The interactions between boundary layer turbulence, including Langmuir turbulence, and submesoscale processes in the oceanic mixed layer are described using large-eddy …