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European tree-ring isotopes indicate unusual recent hydroclimate

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Freund,  Mandy
4.3 Climate Dynamics and Landscape Evolution, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
TERENO, Deutsches GeoForschungsZentrum;

/persons/resource/ghelle

Helle,  G.
4.3 Climate Dynamics and Landscape Evolution, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
TERENO, Deutsches GeoForschungsZentrum;

/persons/resource/balting

Balting,  Daniel
4.3 Climate Dynamics and Landscape Evolution, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;
TERENO, Deutsches GeoForschungsZentrum;

Ballis,  Natasha
External Organizations;
TERENO, Deutsches GeoForschungsZentrum;

Schleser,  Gerhard H.
External Organizations;
TERENO, Deutsches GeoForschungsZentrum;

Cubasch,  Ulrich
External Organizations;
TERENO, Deutsches GeoForschungsZentrum;

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Volltexte (frei zugänglich)

5015343.pdf
(Verlagsversion), 5MB

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Zitation

Freund, M., Helle, G., Balting, D., Ballis, N., Schleser, G. H., Cubasch, U. (2023): European tree-ring isotopes indicate unusual recent hydroclimate. - Communications Earth and Environment, 4, 26.
https://doi.org/10.1038/s43247-022-00648-7


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015343
Zusammenfassung
In recent decades, Europe has experienced more frequent flood and drought events. However, little is known about the long-term, spatiotemporal hydroclimatic changes across Europe. Here we present a climate field reconstruction spanning the entire European continent based on tree-ring stable isotopes. A pronounced seasonal consistency in climate response across Europe leads to a unique, well-verified spatial field reconstruction of European summer hydroclimate back to AD 1600. We find three distinct phases of European hydroclimate variability as possible fingerprints of solar activity (coinciding with the Maunder Minimum and the end of the Little Ice Age) and pronounced decadal variability superimposed by a long-term drying trend from the mid-20th century. We show that the recent European summer drought (2015–2018) is highly unusual in a multi-century context and unprecedented for large parts of central and western Europe. The reconstruction provides further evidence of European summer droughts potentially being influenced by anthropogenic warming and draws attention to regional differences.