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dc.contributor.author Pereira, Rodrigo Kerr Duarte
dc.contributor.author Heywood, Karen
dc.contributor.author Mata, Mauricio Magalhães
dc.contributor.author Garcia, Carlos Alberto Eiras
dc.date.accessioned 2016-01-23T21:28:08Z
dc.date.available 2016-01-23T21:28:08Z
dc.date.issued 2012
dc.identifier.citation PEREIRA, Rodrigo Kerr Duarte et al. On the outflow of dense water from the weddell and ross Seas in OCCAM model.Ocean Science, v. 8, p. 369-388, 2012. Disponível em: <http://www.ocean-sci.net/8/369/2012/os-8-369-2012.pdf>. Acesso em 22 Jan 2016. pt_BR
dc.identifier.issn 2005-7172
dc.identifier.uri http://repositorio.furg.br/handle/1/5867
dc.description.abstract We describe the seasonal and interannual variability of volume transports in the Weddell and Ross Seas using the 1/12◦ 20-yr simulation of the OCCAM global ocean general circulation model. The average simulated full-depth cumulative volume transports were 28.5 ± 2.9 Sv (1 Sv ≡ 106 m3 s −1 ) and 13.4 ± 5.2 Sv, across the main export regions of the Weddell and Ross Seas, respectively. The values of mean outflow of Antarctic Bottom Water (AABW) (defined by neutral density γ n ≥ 28.27 kg m−3 ) from the Weddell and Ross Seas of 10.6 ± 3.1 Sv and 0.5 ± 0.7 Sv, respectively, agree with the range reported in historical observational studies. The export of Weddell Sea dense water in OCCAM is primarily determined by the strength of the Weddell Gyre. Variability in AABW export is predominantly at periods of ∼1 yr and 2–4 yr. pt_BR
dc.language.iso eng pt_BR
dc.rights open access pt_BR
dc.title On the outflow of dense water from the weddell and ross Seas in OCCAM model pt_BR
dc.type article pt_BR
dc.identifier.doi 10.5194/os-8-369-2012 pt_BR


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