Nonlocal closure

From Glossary of Meteorology



nonlocal closure

A method of approximating unknown turbulence quantities, such as covariances, by sums or integrals (over the whole domain of turbulence) of known quantities.

This mimics the effects of a spectrum of eddy sizes causing mixing from various distances. Examples are transilient turbulence theory and spectral diffusivity theory.
See nonlocal flux, nonlocal mixing.


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