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should be included. In some regions, sampling depths need to be increased, so that in addition to upper-ocean heat-content change, the 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 considerable weaknesses in our three-dimensional treatment of the surface layer. Local process models have sometimes shown that small Popular vintage sunflower canvas full printing low top shoeschanges 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

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