[1]The turbulence dissipation rate within the mixed layer was measured in the open ocean and the coastal water of the South China Sea under moderate winds of 4.7 ~ 8.9 m s~(-1) using a free-falling MSS profiler. In the open ocean, the profile of the dissipation rate within the mixed layer exhibited an exponential decay with the depth at most stations, which was satisfactorily consistent with that predicted by the parameterization of wave-turbulence interaction presented by Huang and Qiao (2010) while deviating from that by the law of the wall. In the coastal ocean, however, both the parameterization of wave-turbulence interaction and the law of the wall can give approximate predictions to the measured dissipation rate.
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机译：[1]使用自由落体MSS剖面仪，在4.7〜8.9 m s〜（-1）的中等风向下，在公海和南海沿岸水域中测量了混合层内的湍流耗散率。在公海中，混合层内的耗散率剖面在大多数台站处随深度呈指数衰减，这与Huang和Qiao（2010）提出的波湍流相互作用的参数化所预测的令人满意。根据隔离墙的规律而偏离。然而，在沿海海洋中，波浪湍流相互作用的参数化和壁的定律都可以对测得的耗散率做出近似预测。
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