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Free Content Turbulent Diffusion in the Sea

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The diffusion equations of Goldstein-Michelson and Joseph-Sendner are examined in the light of experimental evidence derived from a Stommel-Richardson-type experiment. It is concluded that the Goldstein-Michelson theory is approximately valid for the small-scale experiment performed, but that modifications may be necessary for a proper description of diffusion from an initially very small to a terminally very large scale. The velocity autocorrelation function implicit in the Goldstein-Michelson theory, if appropriately modified, could be incorporated into a diffusion equation which would describe the empirical increase in diffusivity with increasing scale.

Document Type: Research Article

Publication date: January 1, 1960

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  • The Bulletin of Marine Science is dedicated to the dissemination of high quality research from the world's oceans. All aspects of marine science are treated by the Bulletin of Marine Science, including papers in marine biology, biological oceanography, fisheries, marine affairs, applied marine physics, marine geology and geophysics, marine and atmospheric chemistry, and meteorology and physical oceanography.
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