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Large eddy simulation of the rotation effect on the ocean turbulence kinetic energy budget in the surface mixed layer

Large eddy simulation of the rotation effect on the ocean turbulence kinetic energy budget in the surface mixed layer
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摘要 A non-hydrostatic, Boussinesq, and three-dimensional large eddy simulation(LES) model was used to study the impact of the Earth's rotation on turbulence and the redistribution of energy in turbulence kinetic energy(TKE) budget. A set of numerical simulations was conducted,(1) with and without rotation,(2) at different latitudes(10°N, 30°N, 45°N, 60°N, and 80°N),(3) with wave breaking and with Langmuir circulation, and(4) under different wind speeds(5, 10, 20, and 30 m/s). The results show that eddy viscosity decreases when rotation is included, indicating that rotation weakens the turbulence strength. The TKE budget become tight with rotation and the effects of rotation grow with latitude. However, rotation become less important under Langmuir circulation since the transport term is strong in the vertical direction. Finally, simulations were conducted based on field data from the Boundary Layer and Air-Sea Transfer Low Wind(CBLAST-Low) experiment. The results, although more complex, are consistent with the results obtained from earlier simulations using ideal numerical conditions. A non-hydrostatic, Boussinesq, and three-dimensional large eddy simulation (LES) model was used to study the impact of the Earth's rotation on turbulence and the redistribution of energy in turbulence kinetic energy (TKE) budget. A set of numerical simulations was conducted, (1) with and without rotation, (2) at different latitudes (10°N, 30°N, 45°N, 60°N, and 80°N), (3) with wave breaking and with Langmuir circulation, and (4) under different wind speeds (5, 10, 20, and 30 m/s). The results show that eddy viscosity decreases when rotation is included, indicating that rotation weakens the turbulence strength. The TKE budget become tight with rotation and the effects of rotation grow with latitude. However, rotation become less important under Langmuir circulation since the transport term is strong in the vertical direction. Finally, simulations were conducted based on field data from the Boundary Layer and Air-Sea Transfer Low Wind (CBLAST-Low) experiment. The results, although more complex, are consistent with the results obtained from earlier simulations using ideal numerical conditions.
出处 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2014年第5期1198-1206,共9页 中国海洋湖沼学报(英文版)
基金 Supported by the National Natural Science Foundation of China(Nos.41206015,41106019) the National Basic Research Program of China(973 Program)(Nos.2011CB403501,2012CB417402) the Fund for Creative Research Groups by NSFC(No.41121064)
关键词 large eddy simulation (LES) Earth rotation turbulence kinetic energy (TKE) 大涡模拟 湍流动能 旋转 动能收支 混合层 表面 海洋 数值模拟
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