Show simple item record

dc.contributor.authorGarcía-Serrano, Javier
dc.contributor.authorFrankignoul, C.
dc.contributor.authorKing, M.P.
dc.contributor.authorArribas, A.
dc.contributor.authorGao, Y.
dc.contributor.authorGuemas, Virginie
dc.contributor.authorMatei, D.
dc.contributor.authorMsadek, R.
dc.contributor.authorPark, W.
dc.contributor.authorSanchez-Gomenez, E.
dc.contributor.otherBarcelona Supercomputing Center
dc.date.accessioned2017-11-30T10:31:51Z
dc.date.available2018-10-02T00:30:32Z
dc.date.issued2017-10
dc.identifier.citationGarcía-Serrano, J. [et al.]. Multi-model assessment of linkages between eastern Arctic sea-ice variability and the Euro-Atlantic atmospheric circulation in current climate. "Climate Dynamics", Octubre 2017, vol. 49, núm. 7-8, p. 2407-2429.
dc.identifier.issn0930-7575
dc.identifier.urihttp://hdl.handle.net/2117/111363
dc.description.abstractA set of ensemble integrations from the Coupled Model Intercomparison Project phase 5, with historical forcing plus RCP4.5 scenario, are used to explore if state-of-the-art climate models are able to simulate previously reported linkages between sea-ice concentration (SIC) anomalies over the eastern Arctic, namely in the Greenland–Barents–Kara Seas, and lagged atmospheric circulation that projects on the North Atlantic Oscillation (NAO)/Arctic Oscillation (AO). The study is focused on variability around the long-term trends, so that all anomalies are detrended prior to analysis; the period of study is 1979–2013. The model linkages are detected by applying maximum covariance analysis. As also found in observational data, all the models considered here show a statistically significant link with sea-ice reduction over the eastern Arctic followed by a negative NAO/AO-like pattern. If the simulated relationship is found at a lag of one month, the results suggest that a stratospheric pathway could be at play as the driving mechanism; in observations this is preferentially shown for SIC in November. The interference of a wave-like anomaly over Eurasia, accompanying SIC changes, with the climatological wave pattern appears to be key in setting the mediating role of the stratosphere. On the other hand, if the simulated relationship is found at a lag of two months, the results suggest that tropospheric dynamics are dominant, presumably due to transient eddy feedback; in observations this is preferentially shown for SIC in December. The results shown here and previous evidence from atmosphere-only experiments emphasize that there could be a detectable influence of eastern Arctic SIC variability on mid-latitude atmospheric circulation anomalies. Even if the mechanisms are robust among the models, the timing of the simulated linkages strongly depends on the model and does not generally mimic the observational ones. This implies that the atmospheric sensitivity to sea-ice changes largely depends on the mean-flow and parameterizations, which could lead to misleading conclusions elsewhere if a multi-model ensemble-mean approach is adopted. It might also represent an important source of uncertainty in climate prediction and projection. Modelling efforts are hence further required to improve representation of the background atmospheric circulation and reduce biases, in order to attain more accurate covariability.
dc.description.sponsorshipThe research leading to these results has received funding from the European Union 7th Framework Programme (FP7 2007-2013), under grant agreement No. 308299 (NACLIM—www.naclim.eu). JG-S was partially supported by the H2020-funded MSCA-IF-EF DPETNA project (GA No. 655339). This work was also supported by the BMBF project CLIMPRE Inter-Dec (FKZ:01LP1609A; DM) and the RCN project KLIMAFORSK InterDec (260393; YG) within the framework of JPI CLIM Belmont-Forum InterDec consortial project. JG-S and MPK thank the 6th Severo Ochoa mobility programme for funding the visit of the latter to BSC-CNS in October 2015. The authors thank Ileana Bladé (UB, Spain) and Lantao Sun (CIRES-NOAA/ESRL, USA) for useful discussions, and Neven S. Fuckar (BSC-CNS) for his help during the review process. Technical support at BSC-CNS (Computational Earth Sciences group) is sincerely acknowledged. The authors are also grateful to the anonymous reviewers for their comments, which helped to improve the clarity of the manuscript.
dc.format.extent23 p.
dc.language.isoeng
dc.publisherSpringer
dc.subjectÀrees temàtiques de la UPC::Energies
dc.subject.lcshClimate science
dc.subject.lcshSea ice
dc.subject.lcshAtmospheric circulation
dc.subject.otherArctic sea ice variability
dc.subject.otherNAO/AO pattern
dc.subject.otherAtmospheric teleconnection
dc.titleMulti-model assessment of linkages between eastern Arctic sea-ice variability and the Euro-Atlantic atmospheric circulation in current climate
dc.typeArticle
dc.subject.lemacClima--Observacions
dc.subject.lemacCirculació atmosfèrica
dc.identifier.doi10.1007/s00382-016-3454-3
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://link.springer.com/article/10.1007/s00382-016-3454-3
dc.rights.accessOpen Access
dc.description.versionPostprint (author's final draft)
dc.relation.projectidinfo:eu-repo/grantAgreement/EC/H2020/655339/EU/Dynamics and Predictability of the ENSO teleconnection to the Tropical North Atlantic/DPETNA
dc.relation.projectidinfo:eu-repo/grantAgreement/EC/FP7/308299/EU/North Atlantic Climate: Predictability of the climate in the North Atlantic%2FEuropean sector related to North Atlantic%2FArctic sea surface temperature and sea ice variability and change/NACLIM
upcommons.citation.publishedtrue
upcommons.citation.publicationNameClimate Dynamics
upcommons.citation.volume49
upcommons.citation.number7-8
upcommons.citation.startingPage2407
upcommons.citation.endingPage2429


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

All rights reserved. This work is protected by the corresponding intellectual and industrial property rights. Without prejudice to any existing legal exemptions, reproduction, distribution, public communication or transformation of this work are prohibited without permission of the copyright holder