We discuss the coupling processes between surface gravity waves and adjacent winds and currents in turbulent boundary layers. These processes mediate exchanges of momentum …
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 …
F Ardhuin, L Marié, N Rascle, P Forget… - Journal of physical …, 2009 - journals.ametsoc.org
Observation and Estimation of Lagrangian, Stokes, and Eulerian Currents Induced by Wind and Waves at the Sea Surface in: Journal of Physical Oceanography Volume 39 Issue 11 (2009) …
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 …
The wind-driven stably stratified mid-latitude oceanic surface turbulent boundary layer is computationally simulated in the presence of a specified surface gravity-wave field. The …
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 …
BK Arbic, S Elipot, JM Brasch… - Journal of …, 2022 - Wiley Online Library
The geographical variability, frequency content, and vertical structure of near‐surface oceanic kinetic energy (KE) are important for air‐sea interaction, marine ecosystems …
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 …
ALM Grant, SE Belcher - Journal of Physical Oceanography, 2009 - journals.ametsoc.org
Characteristics of Langmuir Turbulence in the Ocean Mixed Layer in: Journal of Physical Oceanography Volume 39 Issue 8 (2009) Jump to Content Jump to Main Navigation Logo Logo …