Abstract
The distributions of flows and water properties in the world’s oceans exhibit structure on a vast range of space and time scales. The largest scales (of order 107m) are limited chiefly by the size of ocean basins and ultimately of the earth. On the other end of the spectrum, gradients in velocity and water properties exist to sub-meter scales (see below). The total range of spatial scales is thus some nine or more orders of magnitude. The temperature and velocity structures on scales of a few centimeters evolve on a time scale of seconds to minutes (Dillon, 1984); scientists conducting climate studies seek to understand ocean variability on periods of decades to centuries or longer. This gives us in time, a span of at least nine orders of magnitude too. Between these extremes is of course a continuous wavenumber—frequency spectrum of ocean kinetic and potential energy encompassing a host of physical processes (Figure 1). Given these space and time-scale ranges, it is obviously impossible to develop global-scale numerical models that simultaneously resolve all possible oceanographic motions over long times.
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Toole, J.M. (1998). Turbulent Mixing in the Ocean. 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_7
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DOI: https://doi.org/10.1007/978-94-011-5096-5_7
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