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Eric D. Skyllingstad and Simon P. de Szoeke

near the model surface. The LES model is coupled to an ocean model based on the K -profile parameterization (KPP) boundary layer scheme from Large et al. (1994) with momentum nonlocal terms defined as in Smyth et al. (2002) . Each ocean grid point is treated as an independent column that interacts with the LES model grid point. Ocean columns do not exchange properties in the horizontal direction. As shown later in our analysis, lateral gradients of SST and salinity generated by surface flux

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