An important role in climate is played by the surface mixed layer, the upper ocean layer well mixed in ocean properties. Wind stress forcing causes a spiraling Ekman flow in the rotating ocean that decays with depth and transports momentum into the ocean. Con-ventional viewpoint suggests that the wind-driven flow does not penetrate deeper than th
Observations are used to evaluate a simple theoretical model for the generation of near-inertial she...
The near-surface atmosphere layer, and in particular the wind intensity, controls the ocean properti...
A climate model is used to study the climatic impact of the stress exerted on the ocean by the atmos...
The article of record as published may be found at http://dx.doi.org/10.1007/s00024-015-1063-4Classi...
The generation and destruction of stratification in the surface mixed layer of the ocean is understo...
The interaction between the Coriolis force and the Stokes drift associated with ocean surface waves ...
The study of ocean circulation is vital to understanding how our climate works. The movement of the ...
Submesoscale eddies generated by baroclinic instability of upper ocean fronts lead to rapid restrati...
The warming climate influences the ocean by changing its wind‐driven dynamics and by inputting extra...
The one-dimensional bulk mixed-layer model of Niiler (1975) is extended to two (or three) dimensions...
International audienceAbstract The stratification is primarily controlled by temperature in subtropi...
Recent numerical experiments indicate that the rate of meridional overturning associated with North ...
The response of the atmospheric boundary layer to fronts of sea surface temperature (SST) is charact...
Observations are used to evaluate a simple theoretical model for the generation of near-inertial she...
The near-surface atmosphere layer, and in particular the wind intensity, controls the ocean properti...
A climate model is used to study the climatic impact of the stress exerted on the ocean by the atmos...
The article of record as published may be found at http://dx.doi.org/10.1007/s00024-015-1063-4Classi...
The generation and destruction of stratification in the surface mixed layer of the ocean is understo...
The interaction between the Coriolis force and the Stokes drift associated with ocean surface waves ...
The study of ocean circulation is vital to understanding how our climate works. The movement of the ...
Submesoscale eddies generated by baroclinic instability of upper ocean fronts lead to rapid restrati...
The warming climate influences the ocean by changing its wind‐driven dynamics and by inputting extra...
The one-dimensional bulk mixed-layer model of Niiler (1975) is extended to two (or three) dimensions...
International audienceAbstract The stratification is primarily controlled by temperature in subtropi...
Recent numerical experiments indicate that the rate of meridional overturning associated with North ...
The response of the atmospheric boundary layer to fronts of sea surface temperature (SST) is charact...
Observations are used to evaluate a simple theoretical model for the generation of near-inertial she...
The near-surface atmosphere layer, and in particular the wind intensity, controls the ocean properti...
A climate model is used to study the climatic impact of the stress exerted on the ocean by the atmos...