Full Length Research Paper
Abstract
The analysis of the turbulent mixing structure is accomplished by the dynamical computations of the mixing parameters represented by: buoyancy frequency (N), viscous dissipation (ε), turbulent kinetic energy (E), Richardson number (Ri), Reynolds stress, diffusive salt flux (DSF), diffusive heat flux (DHF). In general the computations show that, the water column becomes more stable and less stratified at the deeper layers. Also, the dynamical processes of vertical turbulent mixing are stronger in the surface layers.
Key words: Mediterranean sea, turbulence mixing.
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