... Data . ... 2004 . N . ... . n 1 . ... . ?60 . B z =+12 ?? . ... . . . B z =+10 . ... . ?100 . B z +10 . . ?107 . B z =+15 . ... . ?223 . B z =+37 . . ?110 . B z =+8 |D st | ... APEV . ... . . . B z =+9 . ... - . ... D st ?40 ; . ...
... This assumption is grounded in the classical theory of stationary turbulence in the limit of infinite Reynolds number (e.g. Corrsin, 1951). ... The ratio of diffusivities is obtained as a function of buoyancy Reynolds number Reb and of the density ratio R (the ratio of the contributions of heat and salt to the density stratification). ... The main results are in section 5, where potential energy components, scalar variances and turbulent diffusivities for the two scalars are examined. ...
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