European warm-season temperature and hydroclimate since 850 CE
- Publikationstyp:
- Zeitschriftenaufsatz
- Metadaten:
-
- Autoren
- Fredrik Charpentier Ljungqvist
- Andrea Seim
- Paul J Krusic
- Jesus Fidel Gonzalez-Rouco
- Johannes P Werner
- Edward R Cook
- Eduardo Zorita
- Juerg Luterbacher
- Elena Xoplaki
- Georgia Destouni
- Elena Garcia-Bustainante
- Camilo Andres Melo Aguilar
- Kristina Seftigen
- Jianglin Wang
- Mary H Gagen
- Jan Esper
- Olga Solomina
- Dominik Fleitmann
- Ulf Buntgen
- Autoren-URL
- https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=fis-test-1&SrcAuth=WosAPI&KeyUT=WOS:000478753700002&DestLinkType=FullRecord&DestApp=WOS_CPL
- DOI
- 10.1088/1748-9326/ab2c7e
- Externe Identifier
- Clarivate Analytics Document Solution ID: IN5YU
- ISSN
- 1748-9326
- Ausgabe der Veröffentlichung
- 8
- Zeitschrift
- ENVIRONMENTAL RESEARCH LETTERS
- Schlüsselwörter
- climate variability
- climate model simulations
- gridded climate reconstructions
- hydroclimate
- Europe
- past millennium
- tree-ring data
- Artikelnummer
- ARTN 084015
- Datum der Veröffentlichung
- 2019
- Status
- Published
- Titel
- European warm-season temperature and hydroclimate since 850 CE
- Sub types
- Article
- Ausgabe der Zeitschrift
- 14
Datenquelle: Web of Science (Lite)
- Andere Metadatenquellen:
-
- Abstract
- <jats:title>Abstract</jats:title> <jats:p>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.</jats:p>
- Autoren
- Fredrik Charpentier Ljungqvist
- Andrea Seim
- Paul J Krusic
- Jesús Fidel González-Rouco
- Johannes P Werner
- Edward R Cook
- Eduardo Zorita
- Jürg Luterbacher
- Elena Xoplaki
- Georgia Destouni
- Elena García-Bustamante
- Camilo Andrés Melo Aguilar
- Kristina Seftigen
- Jianglin Wang
- Mary H Gagen
- Jan Esper
- Olga Solomina
- Dominik Fleitmann
- Ulf Büntgen
- DOI
- 10.1088/1748-9326/ab2c7e
- eISSN
- 1748-9326
- Ausgabe der Veröffentlichung
- 8
- Zeitschrift
- Environmental Research Letters
- Online publication date
- 2019
- Paginierung
- 084015 - 084015
- Datum der Veröffentlichung
- 2019
- Status
- Published
- Herausgeber
- IOP Publishing
- Herausgeber URL
- http://dx.doi.org/10.1088/1748-9326/ab2c7e
- Datum der Datenerfassung
- 2021
- Titel
- European warm-season temperature and hydroclimate since 850 CE
- Ausgabe der Zeitschrift
- 14
Datenquelle: Crossref
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