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Turbulent mixing in the springtime central Adriatic Sea (CROSBI ID 120412)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Petrers, Hartmut ; Orlić, Mirko Turbulent mixing in the springtime central Adriatic Sea // Geofizika, 22 (2005), 1-19-x

Podaci o odgovornosti

Petrers, Hartmut ; Orlić, Mirko

engleski

Turbulent mixing in the springtime central Adriatic Sea

A small set of observations of upper ocean turbulent mixing, stratification and currents was obtained in the central Adriatic Sea in May 2003. Owing to light winds, the surface mixed layer was at most 10 m thick and usually much thinner. The water column below was mostly strongly stratified with partially restratified remnant of previous mixed layers. Mesoscale currents were weak with a significant barotropic component. Weak shear and strong stratification tended to combine to large Richardson numbers. Below a layer of enhanced mixing in the upper 10-20 m, eddy diffusivities were mostly small, ranging from 10^-6 m^2 s^-1 to about 5 x 10^-5 m^2 s^-1. Much larger values occurred in a few events, however.

microstructure; turbulence; Adriatic

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Podaci o izdanju

22

2005.

1-19-x

objavljeno

0352-3659

Povezanost rada

Geologija

Indeksiranost