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dc.contributor.authorLjungqvist, Fredrik Charpentier
dc.contributor.authorSeim, Andrea
dc.contributor.authorKrusic, Paul J.
dc.contributor.authorGonzalez-Rouco, Jesus Fidel
dc.contributor.authorWerner, Johannes
dc.contributor.authorCook, Edward R.
dc.contributor.authorZorita, Eduardo
dc.contributor.authorLuterbacher, Jürg
dc.contributor.authorXoplaki, Elena
dc.contributor.authorDestouni, Georgia
dc.contributor.authorGarcia-Bustamante, Elena
dc.contributor.authorAguilar, Camilo Andres Melo
dc.contributor.authorSeftigen, Kristina
dc.contributor.authorWang, Jianglin
dc.contributor.authorGagen, Mary H.
dc.contributor.authorEsper, Jan
dc.contributor.authorSolomina, Olga
dc.contributor.authorFleitmann, Dominik
dc.contributor.authorBüntgen, Ulf
dc.date.accessioned2021-02-24T09:56:26Z
dc.date.available2021-02-24T09:56:26Z
dc.date.created2020-03-16T17:13:09Z
dc.date.issued2019
dc.identifier.issn1748-9326
dc.identifier.urihttps://hdl.handle.net/11250/2729998
dc.description.abstractThe long-term relationship between temperature and hydroclimate has remained uncertain due to the short length of instrumental measurements and inconsistent results from climate model simulations. This lack of understanding is particularly critical with regard to projected drought and flood risks. Here we assess warm-season co-variability patterns between temperature and hydroclimate over Europe back to 850 CE using instrumental measurements, tree-ring based reconstructions, and climate model simulations. We find that the temperature–hydroclimate relationship in both the instrumental and reconstructed data turns more positive at lower frequencies, but less so in model simulations, with a dipole emerging between positive (warm and wet) and negative (warm and dry) associations in northern and southern Europe, respectively. Compared to instrumental data, models reveal a more negative co-variability across all timescales, while reconstructions exhibit a more positive co-variability. Despite the observed differences in the temperature–hydroclimate co-variability patterns in instrumental, reconstructed and model simulated data, we find that all data types share relatively similar phase-relationships between temperature and hydroclimate, indicating the common influence of external forcing. The co-variability between temperature and soil moisture in the model simulations is overestimated, implying a possible overestimation of temperature-driven future drought risks.en_US
dc.language.isoengen_US
dc.publisherIOP Publishingen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleEuropean warm-season temperature and hydroclimate since 850 CEen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2019 The Author(s).en_US
dc.source.articlenumber084015en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.1088/1748-9326/ab2c7e
dc.identifier.cristin1801905
dc.source.journalEnvironmental Research Lettersen_US
dc.source.4014
dc.source.148
dc.identifier.citationEnvironmental Research Letters. 2019, 14 (8), 084015.en_US
dc.source.volume14en_US
dc.source.issue8en_US


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal