Abstract
The practice of oceanic numerical modeling is growing rapidly. Among the reasons for this are the following: a widespread realization that model solutions can, either now or at least in the near future, be skillful in mimicking observed oceanic features; an understanding of the limitations of the alternative and more traditional scientific methodologies of making measurements in the oceans and developing analytic theories for highly nonlinear dynamical systems; an appreciation of the importance of the oceans in the socially compelling problems of anthropogenic changes in climate and the environment; and an exploitation of the steady increases in computing power that make meaningfully comprehensive oceanic calculations ever more feasible.
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McWilliams, J.C. (1998). Oceanic General Circulation Models. In: Chassignet, E.P., Verron, J. (eds) Ocean Modeling and Parameterization. NATO Science Series, vol 516. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5096-5_1
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