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DOI10.1088/1748-9326/ab2c7e
European warm-season temperature and hydroclimate since 850 CE
Ljungqvist F.C.; Seim A.; Krusic P.J.; González-Rouco J.F.; Werner J.P.; Cook E.R.; Zorita E.; Luterbacher J.; Xoplaki E.; Destouni G.; García-Bustamante E.; Aguilar C.A.M.; Seftigen K.; Wang J.; Gagen M.H.; Esper J.; Solomina O.; Fleitmann D.; Büntgen U.
发表日期2019
ISSN17489318
卷号14期号:8
英文摘要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. © 2019 The Author(s). Published by IOP Publishing Ltd.
英文关键词climate model simulations; climate variability; Europe; gridded climate reconstructions; hydroclimate; past millennium; tree-ring data
语种英语
scopus关键词Drought; Floods; Forestry; Repair; Soil moisture; Trees (mathematics); Climate model simulations; Climate reconstruction; Climate variability; Europe; hydroclimate; past millennium; Tree ring data; Climate models; climate modeling; climate variation; dendroclimatology; drought stress; flooding; proxy climate record; reconstruction; soil moisture; tree ring
来源期刊Environmental Research Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/154460
作者单位Department of History, Stockholm University, Stockholm, Sweden; Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden; Department of Geography, University of Cambridge, Cambridge, United Kingdom; Department of Forest Growth and Dendroecology, Institute of Forest Sciences, University of Freiburg, Freiburg, Germany; Department of Physical Geography, Stockholm University, Stockholm, Sweden; Department of Physics of the Earth and Astrophysics, IGEO (UCM-CSIC), Universidad Complutense de Madrid, Madrid, Spain; Bjerknes Centre for Climate Research, University of Bergen, Bergen, Norway; Lamont-Doherty Earth Observatory, Columbia University, Palisades, United States; Helmholtz-Zentrum Geesthacht, Institute for Coastal Research, Geesthacht, Germany; Department of Geography, Climatology, Climate Dynamics and Climate Change, Justus Liebig University Giessen, Giessen, Germany; Centre for International Development and Environmental Research, Justus Liebig University Giessen, Giessen, Germany; Unid...
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Ljungqvist F.C.,Seim A.,Krusic P.J.,et al. European warm-season temperature and hydroclimate since 850 CE[J],2019,14(8).
APA Ljungqvist F.C..,Seim A..,Krusic P.J..,González-Rouco J.F..,Werner J.P..,...&Büntgen U..(2019).European warm-season temperature and hydroclimate since 850 CE.Environmental Research Letters,14(8).
MLA Ljungqvist F.C.,et al."European warm-season temperature and hydroclimate since 850 CE".Environmental Research Letters 14.8(2019).
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