Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Ozgokmen T.M. 3"'
Publikováno v:
Journal of marine research
62 (2004): 1–35.
info:cnr-pdr/source/autori:Griffa A. (1), Piterbarg L.I. (2), Ozgokmen T.M. (3)/titolo:Predictability of Lagrangian particle trajectories: effects of uncertainty in the underlying Eulerian flow/doi:/rivista:Journal of marine research (Print)/anno:2004/pagina_da:1/pagina_a:35/intervallo_pagine:1–35/volume:62
62 (2004): 1–35.
info:cnr-pdr/source/autori:Griffa A. (1), Piterbarg L.I. (2), Ozgokmen T.M. (3)/titolo:Predictability of Lagrangian particle trajectories: effects of uncertainty in the underlying Eulerian flow/doi:/rivista:Journal of marine research (Print)/anno:2004/pagina_da:1/pagina_a:35/intervallo_pagine:1–35/volume:62
The increasing realism of ocean circulation models is leading to an increasing use of Eulerian models as a basis to compute transport properties and to predict the fate of Lagrangian quantities. There exists, however, a significant gap between the sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::aea6e44e51a87e71609ca2dd3d556119
https://publications.cnr.it/doc/49181
https://publications.cnr.it/doc/49181
Publikováno v:
Journal of marine systems 36 (2002): 219–238.
info:cnr-pdr/source/autori:Molcard A. 1, Gervasio L. 1., Griffa A. 1, Gasparini G.P. 1, Mortier L. 2, Ozgokmen T.M. 3/titolo:Numerical investigation of the Sicily Channel dynamics: density currents and water mass advection/doi:/rivista:Journal of marine systems/anno:2002/pagina_da:219/pagina_a:238/intervallo_pagine:219–238/volume:36
info:cnr-pdr/source/autori:Molcard A. 1, Gervasio L. 1., Griffa A. 1, Gasparini G.P. 1, Mortier L. 2, Ozgokmen T.M. 3/titolo:Numerical investigation of the Sicily Channel dynamics: density currents and water mass advection/doi:/rivista:Journal of marine systems/anno:2002/pagina_da:219/pagina_a:238/intervallo_pagine:219–238/volume:36
The Sicily Channel connects the western and eastern Mediterranean sub-basins, playing a fundamental role in the dynamics of the Mediterranean circulation. The flow in the Channel is driven by direct forcing such as wind and by thermohaline processes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::d4ec1b859534c96f553a936414afe41d
http://www.cnr.it/prodotto/i/48915
http://www.cnr.it/prodotto/i/48915