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  • Charpentier Ljungqvist, FredrikStockholms universitet,Historiska institutionen,University of Cambridge, United Kingdom (author)

European warm-season temperature and hydroclimate since 850 CE

  • Article/chapterEnglish2019

Publisher, publication year, extent ...

  • 2019-07-29
  • IOP Publishing,2019

Numbers

  • LIBRIS-ID:oai:gup.ub.gu.se/283060
  • https://gup.ub.gu.se/publication/283060URI
  • https://doi.org/10.1088/1748-9326/ab2c7eDOI
  • https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-171966URI

Supplementary language notes

  • Language:English

Part of subdatabase

Classification

  • Subject category:ref swepub-contenttype
  • Subject category:art swepub-publicationtype

Notes

  • The 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.

Subject headings and genre

Added entries (persons, corporate bodies, meetings, titles ...)

  • Seim, A. (author)
  • Krusic, Paul J.Stockholms universitet,Institutionen för naturgeografi,University of Cambridge, United Kingdom(Swepub:su)pakru (author)
  • Gonzalez-Rouco, J. F. (author)
  • Werner, J. P. (author)
  • Cook, E. R. (author)
  • Zorita, E. (author)
  • Luterbacher, J. (author)
  • Xoplaki, E. (author)
  • Destouni, GeorgiaStockholms universitet,Institutionen för naturgeografi(Swepub:su)gdest (author)
  • Garcia-Bustainante, E. (author)
  • Aguilar, C. A. M. (author)
  • Seftigen, Kristina,1985Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences(Swepub:gu)xsefkr (author)
  • Wang, J. L. (author)
  • Gagen, M. H. (author)
  • Esper, J. (author)
  • Solomina, O. (author)
  • Fleitmann, D. (author)
  • Buntgen, U. (author)
  • Stockholms universitetHistoriska institutionen (creator_code:org_t)

Related titles

  • In:Environmental Research Letters: IOP Publishing14:81748-9326

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