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The warmer the ocean surface, the shallower the mixed layer. How much of this is true?

dc.contributor.authorSomavilla Cabrillo, Raquel
dc.contributor.authorGonzález-Pola Muñiz, César Manuel
dc.contributor.authorFernández Díaz, Julio Manuel 
dc.date.accessioned2018-02-06T10:11:22Z
dc.date.available2018-02-06T10:11:22Z
dc.date.issued2017
dc.identifier.citationJournal of Geophysical Research: Oceans, 122(9), p. 7698-7716 (2017); doi:10.1002/2017JC013125
dc.identifier.issn2169-9275
dc.identifier.urihttp://hdl.handle.net/10651/45507
dc.description.sponsorshipR. Somavilla is supported by a Marie Curie Cların Cofund grant (AC B-1431). Support for this study was provided by the Principado de Asturias (GRUPIN14-144: GIDEP: Grupo de Investigacion de Dinamica del Ecosistema Planctonico)
dc.format.extentp. 7698-7716
dc.language.isoeng
dc.relation.ispartofJournal of Geophysical Research: Oceans
dc.rights© 2017. The Authors
dc.rightsCC Reconocimiento - No comercial - Sin obras derivadas 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.sourceScopus
dc.source.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85030170251&doi=10.1002%2f2017JC013125&partnerID=40&md5=30e86dcf83a65bb8b6a61c1d06b2d1e2
dc.titleThe warmer the ocean surface, the shallower the mixed layer. How much of this is true?eng
dc.typejournal article
dc.identifier.doi10.1002/2017JC013125
dc.relation.projectIDMarie Curie Cların Cofund/AC B-1431
dc.relation.projectIDPrincipado de Asturias/GRUPIN14-144
dc.relation.publisherversionhttp://dx.doi.org/10.1002/2017JC013125
dc.rights.accessRightsopen access


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© 2017. The Authors
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