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dc.contributor.authorLlanillo, P. J.-
dc.contributor.authorPelegrí, Josep Lluís-
dc.contributor.authorTalley, L.-
dc.contributor.authorPeña-Izquierdo, Jesús-
dc.contributor.authorCordero, J.-
dc.date.accessioned2018-05-31T11:40:37Z-
dc.date.available2018-05-31T11:40:37Z-
dc.date.issued2018-03-
dc.identifierdoi: 10.1002/2017JC013509-
dc.identifierissn: 2169-9291-
dc.identifiere-issn: 2169-9291-
dc.identifier.citationJournal of Geophysical Research: Oceans 123(3): 1722-1744 (2018)-
dc.identifier.urihttp://hdl.handle.net/10261/165427-
dc.description23 pages, 9 figures, 3 tables, supporting information https://doi.org/10.1002/2017JC013509-
dc.description.abstractVentilation of the eastern South Pacific Oxygen Minimum Zone (ESP-OMZ) is quantified using climatological Argo and dissolved oxygen data, combined with reanalysis wind stress data. We (1) estimate all oxygen fluxes (advection and turbulent diffusion) ventilating this OMZ, (2) quantify for the first time the oxygen contribution from the subtropical versus the traditionally studied tropical-equatorial pathway, and (3) derive a refined annual-mean oxygen budget for the ESP-OMZ. In the upper OMZ layer, net oxygen supply is dominated by tropical-equatorial advection, with more than one-third of this supply upwelling into the Ekman layer through previously unevaluated vertical advection, within the overturning component of the regional Subtropical Cell (STC). Below the STC, at the OMZ's core, advection is weak and turbulent diffusion (isoneutral and dianeutral) accounts for 89% of the net oxygen supply, most of it coming from the oxygen-rich subtropical gyre. In the deep OMZ layer, net oxygen supply occurs only through turbulent diffusion and is dominated by the tropical-equatorial pathway. Considering the entire OMZ, net oxygen supply (3.84 ± 0.42 µmol kg yr) is dominated by isoneutral turbulent diffusion (56.5%, split into 32.3% of tropical-equatorial origin and 24.2% of subtropical origin), followed by isoneutral advection (32.0%, split into 27.6% of tropical-equatorial origin and 4.4% of subtropical origin) and dianeutral diffusion (11.5%). One-quarter (25.8%) of the net oxygen input escapes through dianeutral advection (most of it upwelling) and, assuming steady state, biological consumption is responsible for most of the oxygen loss (74.2%)-
dc.description.sponsorshipP.J. Llanillo acknowledges support from CONICYT/FONDECYT through the Postdoctorado project 3150229. J.L. Pelegrí and J. Peña-Izquierdo acknowledge funding by the Spanish Ministerio de Economía y Competitividad through projects TIC-MOC (CTM2011-28867) and VA-DE-RETRO (CTM2014-56987-P)-
dc.publisherAmerican Geophysical Union-
dc.relationMINECO/ICTI2013-2016/CTM2014-56987-P-
dc.relation.isversionofPublisher's version-
dc.rightsopenAccessen_EN
dc.titleOxygen Pathways and Budget for the Eastern South Pacific Oxygen Minimum Zone-
dc.typeartículo-
dc.relation.publisherversionhttps://doi.org/10.1002/2017JC013509-
dc.embargo.terms2018-10-01-
dc.date.updated2018-05-31T11:40:38Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.rights.licensehttps://publications.agu.org/open-access/-
dc.contributor.funderMinisterio de Economía y Competitividad (España)-
dc.contributor.funderComisión Nacional de Investigación Científica y Tecnológica (Chile)-
dc.contributor.funderFondo Nacional de Desarrollo Científico y Tecnológico (Chile)-
dc.relation.csic-
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002850es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002848es_ES
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