Abstract
Abstract A method for evaluating the utility of a given parameterization field in a spatially inhomogeneous circulation is described. This method is used to examine the mean field diffusion parameterization of the heat, momentum and vorticity time deviation eddy terms from a mesoscale resolution numerical ocean circulation experiment. The diffusion model does not satisfactorily describe the eddy terms for any field throughout any of the different regions of the model flow.
Cite
CITATION STYLE
Harrison, D. E. (1978). On the Diffusion Parameterization of Mesoscale Eddy Effects from a Numerical Ocean Experiment. Journal of Physical Oceanography, 8(5), 913–918. https://doi.org/10.1175/1520-0485(1978)008<0913:otdpom>2.0.co;2
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