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dc.rights.licenseopenen_US
hal.structure.identifierMax Planck Institute for Meteorology [MPI-M]
hal.structure.identifierUniversità Iuav di Venezia = Iuav University of Venice [IUAV]
dc.contributor.authorZANCHETTIN, Davide
hal.structure.identifierClimate Service Center [Hambourg] [GERICS]
dc.contributor.authorBOTHE, O.
hal.structure.identifierUniversität Bern / University of Bern [UNIBE]
dc.contributor.authorLEHNER, Flavio
hal.structure.identifierProcessus de la variabilité climatique tropicale et impacts [PARVATI]
dc.contributor.authorORTEGA, Pablo
hal.structure.identifierUniversität Bern / University of Bern [UNIBE]
dc.contributor.authorRAIBLE, C.C.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
dc.date.accessioned2024-06-19T08:38:02Z
dc.date.available2024-06-19T08:38:02Z
dc.date.issued2015-06-24
dc.identifier.issn1814-9324en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200573
dc.description.abstractEnReconstructions of past climate behavior often describe prominent anomalous periods that are not necessarily captured in climate simulations. Here, we illustrate the contrast between an interdecadal strong positive phase of the winter Pacific/North American pattern (PNA) in the early 19th century that is described by a PNA reconstruction based on tree rings from northwestern North America, and a slight tendency towards negative winter PNA anomalies during the same period in an ensemble of state-of-the-art coupled climate simulations. Additionally, a pseudo-proxy investigation with the same simulation ensemble allows for assessing the robustness of PNA reconstructions using solely geophysi-cal predictors from northwestern North America for the last millennium. The reconstructed early 19th-century positive PNA anomaly emerges as a potentially reliable feature, although the pseudo-reconstructions are subject to a number of sources of uncertainty and deficiencies highlighted especially at multidecadal and centennial timescales. The pseudo-reconstructions demonstrate that the early 19th-century discrepancy between reconstructed and simulated PNA does not stem from the reconstruction process. Instead, reconstructed and simulated features of the early 19th-century PNA can be reconciled by interpreting the reconstructed evolution during this time as an expression of internal climate variability, which is unlikely to be reproduced in its exact temporal occurrence by a small ensemble of climate simulations. However , firm attribution of the reconstructed PNA anomaly is hampered by known limitations and deficiencies of coupled climate models and uncertainties in the early 19th-century external forcing and background climate state.
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.title.enReconciling reconstructed and simulated features of the winter Pacific/North American pattern in the early 19th century
dc.typeArticle de revueen_US
dc.identifier.doi10.5194/cp-11-939-2015en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
bordeaux.journalClimate of the Pasten_US
bordeaux.page939-958en_US
bordeaux.volume11en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01259469
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Climate%20of%20the%20Past&rft.date=2015-06-24&rft.volume=11&rft.issue=6&rft.spage=939-958&rft.epage=939-958&rft.eissn=1814-9324&rft.issn=1814-9324&rft.au=ZANCHETTIN,%20Davide&BOTHE,%20O.&LEHNER,%20Flavio&ORTEGA,%20Pablo&RAIBLE,%20C.C.&rft.genre=article


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