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Publikováno v:
28C (2005): 33–54.
info:cnr-pdr/source/autori:Carniel S. (1), Sclavo M. (1), Kantha L.H. (2), Clayson C.A. (3)/titolo:Langmuir cells and mixing in the upper ocean/doi:/rivista:/anno:2005/pagina_da:33/pagina_a:54/intervallo_pagine:33–54/volume:28C
info:cnr-pdr/source/autori:Carniel S. (1), Sclavo M. (1), Kantha L.H. (2), Clayson C.A. (3)/titolo:Langmuir cells and mixing in the upper ocean/doi:/rivista:/anno:2005/pagina_da:33/pagina_a:54/intervallo_pagine:33–54/volume:28C
The presence of surface gravity waves at the ocean surface has two important effects on turbulence in the oceanic mixed layer (ML): the wave breaking and the Langmuir cells (LC). Both these effects act as additional sources of turbulent kinetic energ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::fa3d894127dc1568309a241b9ddbefab
http://www.cnr.it/prodotto/i/48940
http://www.cnr.it/prodotto/i/48940