Eddy resolution versus eddy diffusion in a double gyre GCM. Part II: mixing of passive tracers

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Abstract

The coarse-resolution tracer simulations presented here indicate that there is no eddy diffusivity field consistently determined that when combined with a coarse advective velocity field can totally reproduce the tracer distribution and the meridional tracer fluxes comparable to those obtained from the eddy-resolving version of the model. However, the use of a spatially dependent horizontal diffusivity field greatly improves the accuracy of the passive tracer simulations (compared to the eddy-resolving simulations) over the use of a constant eddy diffusion coefficient. -from Author

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Figueroa, H. A. (1994). Eddy resolution versus eddy diffusion in a double gyre GCM. Part II: mixing of passive tracers. Journal of Physical Oceanography, 24(2), 387–402. https://doi.org/10.1175/1520-0485(1994)024<0387:ERVEDI>2.0.CO;2

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