Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Munk's ocean model"'
Autor:
Paulo S. Polito, Olga T. Sato, Dante C. Napolitano, Iury T. Simoes-Sousa, Hélio Almeida, Fabrício R. Lapolli
Publikováno v:
Ocean and Coastal Research, Vol 69 (2022)
At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk’s circulation theory aided by a Lagrangian particl
Externí odkaz:
https://doaj.org/article/a5854bbe493746369595b996872f0c90
Autor:
Polito, Paulo S., Sato, Olga T., Napolitano, Dante C., Simoes-Sousa, Iury T., Almeida, Hélio, Lapolli, Fabrício R.
Publikováno v:
Ocean and Coastal Research, Volume: 69, Article number: e21011, Published: 09 AUG 2021
At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk's circulation theory aided by a Lagrangian particles
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______608::8cec9a96f083786f13982f8f8cae0d11
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2675-28242021000100800&lng=en&tlng=en
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2675-28242021000100800&lng=en&tlng=en
Akademický článek
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Autor:
Crisciani, F., Purini, R.
Publikováno v:
European Physical Journal B: Condensed Matter; Feb2003, Vol. 31 Issue 4, p571-575, 5p, 1 Graph
Autor:
F. Crisciani, R. Purini
Publikováno v:
31 (2003): 571–575.
info:cnr-pdr/source/autori:Crisciani F. 1, Purini R. 1/titolo:A note on the dynamic boundary conditions in Munk-like circulation models/doi:/rivista:/anno:2003/pagina_da:571/pagina_a:575/intervallo_pagine:571–575/volume:31
info:cnr-pdr/source/autori:Crisciani F. 1, Purini R. 1/titolo:A note on the dynamic boundary conditions in Munk-like circulation models/doi:/rivista:/anno:2003/pagina_da:571/pagina_a:575/intervallo_pagine:571–575/volume:31
The present note deals with Munk's ocean model and proposes an alternative approach to find its solution, with special regard to the western boundary layer. We introduce a suitable "distance" between the related Sverdrup streamfunction and all the ad