Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Dynamics of the upper ocean"'
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
Autor:
Crisciani F. (1), Cavallini F. (2)
Publikováno v:
28C (2005): 881–891.
info:cnr-pdr/source/autori:Crisciani F. (1), Cavallini F. (2)/titolo:The no-slip condition at the western boundary of a homogeneous ocean minimizes energy/doi:/rivista:/anno:2005/pagina_da:881/pagina_a:891/intervallo_pagine:881–891/volume:28C
info:cnr-pdr/source/autori:Crisciani F. (1), Cavallini F. (2)/titolo:The no-slip condition at the western boundary of a homogeneous ocean minimizes energy/doi:/rivista:/anno:2005/pagina_da:881/pagina_a:891/intervallo_pagine:881–891/volume:28C
It is not obvious, a priori, that the no-slip boundary condition is suitable for ocean circulation models based on quasi-geostrophic equations. But the no-slip condition is the one that minimizes the kinetic energy of the western boundary layer of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a2e82b4bab0b7ba50e7c59fe18cd1cc9
https://publications.cnr.it/doc/48944
https://publications.cnr.it/doc/48944
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