Large-Eddy Simulation of a Coastal Ocean under the Combined Effects of Surface Heat Fluxes and Full-Depth Langmuir Circulation
| Autor: | Rachel Walker, Chester E. Grosch, Andres E. Tejada-Martinez |
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| Rok vydání: | 2016 |
| Předmět: |
Buoyancy
010504 meteorology & atmospheric sciences Langmuir Turbulence Mixed layer Stratification (water) engineering.material Oceanography Atmospheric sciences 01 natural sciences Wind speed 010305 fluids & plasmas Surface wave 0103 physical sciences engineering Significant wave height Geology 0105 earth and related environmental sciences Langmuir circulation |
| Zdroj: | Journal of Physical Oceanography. 46:2411-2436 |
| ISSN: | 1520-0485 0022-3670 |
| Popis: | Results are presented from the large-eddy simulations (LES) of a wind-driven flow representative of the shallow coastal ocean under the influences of Langmuir forcing and surface heating and cooling fluxes. Langmuir (wind and surface gravity wave) forcing leads to the generation of Langmuir turbulence consisting of a wide range of Langmuir circulations (LCs) or parallel, counterrotating vortices that are aligned roughly in the direction of the wind. In unstratified, shallow coastal regions, the largest of the LCs reach the bottom of the water column. Full-depth LCs are investigated under surface waves with a significant wave height of 1.2 m and a dominant wavelength of 90 m and wave period of 8 s, for a wind speed of 7.8 m s−1 in a 15-m-deep coastal shelf region. Both unstable and stable stratification are imposed by constant surface heat fluxes and an adiabatic bottom wall. Simulations are characterized by Rayleigh and Richardson numbers representative of surface buoyancy forcing relative to wind forcing. For the particular combination of Langmuir forcing parameters studied, although surface cooling is able to augment the strength of LC, a significantly high cooling flux of 560 W m−2 (such that the Rayleigh number is Raτ = 1000) is required in order for turbulence kinetic energy generation by convection to exceed Langmuir production. Such a transition is expected at a lower heat flux for weaker wind and wave conditions and thus weaker LCs than those studied. Furthermore, a surface heating flux of approximately 281 W m−2 (such that the Richardson number is Riτ = 500) is able to inhibit vertical mixing of LC, particularly in the bottom half of the water column, allowing stable stratification to develop. |
| Databáze: | OpenAIRE |
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