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Lack of bipolar see-saw in response to Southern Ocean wind reduction

dc.contributor.authorLevermann, A.
dc.contributor.authorSchewe, J.
dc.contributor.authorMontoya Redondo, María Luisa
dc.date.accessioned2023-06-20T11:15:52Z
dc.date.available2023-06-20T11:15:52Z
dc.date.issued2007-06-28
dc.description© 2007 by the American Geophysical Union. We are grateful to J. R. Toggweiler and J. Mignot for useful comments on the manuscript. A.L. was funded by the Gary Comer foundation, M.M. by the Ramón y Cajal Program and project CGL2005-06097/CLI of the Spanish Ministry for Science and Education.
dc.description.abstractA cessation of the Atlantic meridional overturning circulation (AMOC) significantly reduces northward oceanic heat transport. In response to anomalous freshwater flux, this leads to the classic 'bipolar see-saw' pattern of northern cooling and southern warming in surface air and ocean temperatures. By contrast, as shown here in a coupled climate model, both northern and southern cooling are observed for an AMOC reduction in response to reduced wind stress in the Southern Ocean (SO). For very weak SO wind stress, not only the overturning circulation collapses, but sea ice export from the SO is strongly reduced. Consequently, sea ice extent and albedo increase in this region. The resulting cooling overcompensates the warming by the reduced northward heat transport. The effect depends continuously on changes in wind stress and is reversed for increased winds. It may have consequences for abrupt climate change, the last deglaciation and climate sensitivity to increasing atmospheric CO_2 concentration.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipComer Family Foundation
dc.description.sponsorshipAyudas para contratos Ramón y Cajal (RYC)
dc.description.sponsorshipMinisterio de Educación y Ciencia (MEC), España
dc.description.sponsorshipMinisterio de Economía y Competitividad (MINECO), España
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/37940
dc.identifier.doi10.1029/2007GL030255
dc.identifier.issn0094-8276
dc.identifier.officialurlhttp://dx.doi.org/10.1029/2007GL030255
dc.identifier.relatedurlhttp://onlinelibrary.wiley.com/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/51893
dc.issue.number12
dc.journal.titleGeophysical research letters
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.relation.projectIDCGL2005-06097/CLI
dc.rights.accessRightsopen access
dc.subject.cdu52
dc.subject.keywordMeridional overturning circulation
dc.subject.keywordThermohaline circulation
dc.subject.keywordClimate-change
dc.subject.keywordIntermediate complexity
dc.subject.keyword2nd-order moments
dc.subject.keywordHemisphere winds
dc.subject.keywordSystem model
dc.subject.keywordPerformance
dc.subject.keywordGreenland
dc.subject.keywordSensitivity
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.titleLack of bipolar see-saw in response to Southern Ocean wind reduction
dc.typejournal article
dc.volume.number34
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