Mixing driven by vertically variable forcing: an application to the case of Langmuir circulation
From MaRDI portal
Publication:4350977
DOI10.1017/S0022112096002716zbMath0888.76027OpenAlexW2148096066WikidataQ58390442 ScholiaQ58390442MaRDI QIDQ4350977
Publication date: 13 May 1998
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112096002716
Rayleigh numberwave-current interaction40 mode Galerkin expansiondepth-averaged forcingfinite amplitude cellsLangmuir cellsoceanic mixed layers
Hydrology, hydrography, oceanography (86A05) Stability and instability of geophysical and astrophysical flows (76E20)
Cites Work
- Finite amplitude cellular convection
- The effect of Langmuir circulation on the distribution of submerged bubbles caused by breaking wind waves
- Large-scale flow in turbulent convection: a mathematical model
- Nonlinear dynamics in Langmuir circulations and in thermosolutal convection
- The instability of the ocean to Langmuir circulations
- A rational model for Langmuir circulations
- On the evolution of the system of wind drift currents and Langmuir circulations in the ocean. Part 1. Theory and averaged current
- On surface drift currents in the ocean
- A wave-interaction model for the generation of windrows
This page was built for publication: Mixing driven by vertically variable forcing: an application to the case of Langmuir circulation