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Jody M. Klymak

studies are planned to try to predict the low-wavenumber drag over the stochastic topography better and to incorporate it into numerical models so that drag is not double counted. The importance of getting this parameterization correct is an open question. Models that are freely running (with no data assimilation) must have bottom stresses that are adequate to balance the externally imposed surface wind stress. If the bottom drag is conceptualized as quadratic with the near-bottom flows, then having

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