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Sue Chen, Maria Flatau, Tommy G. Jensen, Toshiaki Shinoda, Jerome Schmidt, Paul May, James Cummings, Ming Liu, Paul E. Ciesielski, Christopher W. Fairall, Ren-Chieh Lien, Dariusz B. Baranowski, Nan-Hsun Chi, Simon de Szoeke, and James Edson

sigma levels wherein 20 levels were assigned within the lowest 2 km of the atmosphere. The Navy Coastal Ocean Model (NCOM; Martin 2000 ) is run using a horizontal resolution of 12 km with 60 sigma- z vertical layers. A fine vertical spacing (0.5 m) is used in the upper 10 m to resolve the large diurnal warming features ( Shinoda et al. 2013 ). The vertical mixing is modified to include Stokes drift currents provided by a wave model and effects of Langmuir circulations ( Smith et al. 2013 ). d

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