Diapycnal eddy diffusivity: Difference between revisions

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{{DefineConcept
{{DefineConcept
|parameter_name=Diapycnal eddy diffusivity <math>K_\rho</math>
|parameter_name=Diapycnal eddy diffusivity <math>K_\rho</math>
|description=Diapycnal eddy diffusivity (for buoyancy) is defined from the buoyancy flux <math>\overline{w'\rho'}</math>
|description=Diapycnal eddy diffusivity (for buoyancy) is defined from the buoyancy flux <math>\overline{w'\rho'}</math> and the background density gradient <math>\frac{\partial\rho}{\partial z}</math>
|article_type=Concept
|article_type=Concept
|instrument_type=Velocity profilers
|instrument_type=Velocity profilers
}}
}}
Osborn 1980 showed that <math>K_\rho =\frac{\bar{w'\rho'}}{\partial \rho/\partial z}\Gamma \epsilon N^{-2}</math>
Osborn 1980 showed that <math>K_\rho =\frac{\bar{w'\rho'}}{\partial \rho/\partial z}\Gamma \epsilon N^{-2}</math>

Revision as of 13:39, 14 October 2021


Short definition of Diapycnal eddy diffusivity (Diapycnal eddy diffusivity Kρ)
Diapycnal eddy diffusivity (for buoyancy) is defined from the buoyancy flux wρ and the background density gradient ρz

This is the common definition for Diapycnal eddy diffusivity, but other definitions maybe discussed within the wiki.

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Osborn 1980 showed that Kρ=wρ¯ρ/zΓϵN2