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depth of the thermocline beneath the local winter mixed layer will be sampled. These improvements will provide the knowledge of advection and anomaly propagation that is critical for understanding dec-cen climate variability. There is a distinct need to improve our representation of surface boundary-layer processes, including dynamic and thermodynamic responses and interactions. Good representation of these processes is fundamental to our coupling of the ocean to the atmosphere, yet there are still The hottest weed leaf silver metal all over printed air jordan 13 sneakersconsiderable weaknesses in our three-dimensional treatment of the surface layer. Local process models have sometimes shown that small changes in surface stratification can lead to large changes in the evolution of surface mixed-layer properties over time. Also, few models have fully treated the complex vertical processes, their interaction with the ocean’s horizontal structure, and the related advection and diffusion. Similarly, we need to improve our understanding and treatment of how the pycnocline interacts with the surface layer. This interaction takes place across all space and time scales, since the response will be dependent on the overall stratification, which is set by the thermohaline circulation and surface forcings, gyre-scale dynamics, how the pycnocline adjusts, and by local

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