Consistent multidecadal variability in global temperature reconstructions and simulations over the Common Era
Multidecadal surface temperature changes may be forced by natural as well as anthropogenic factors, or arise unforced from the climate system. Distinguishing these factors is essential for estimating sensitivity to multiple climatic forcings and the amplitude of the unforced variability. Here we pre...
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
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24 July 2019
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Nature geoscience
Year: 2019, Jahrgang: 12, Heft: 8, Pages: 643-649 |
| ISSN: | 1752-0908 |
| DOI: | 10.1038/s41561-019-0400-0 |
| Online-Zugang: | Verlag, Volltext: https://doi.org/10.1038/s41561-019-0400-0 Verlag, Volltext: https://www.nature.com/articles/s41561-019-0400-0 
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| Verfasserangaben: | PAGES 2k Consortium: Raphael Neukom, Luis A. Barboza, Michael P. Erb, Feng Shi, Julien Emile-Geay, Michael N. Evans, Jorg Franke, Darrell S. Kaufman, Lucie Lucke, Kira Rehfeld, Andrew Schurer, Feng Zhu, Stefan Bronnimann, Gregory J. Hakim, Benjamin J. Henley, Fredrik Charpentier Ljungqvist, Nicholas McKay, Veronika Valler, Lucien von Gunten |
| Zusammenfassung: | Multidecadal surface temperature changes may be forced by natural as well as anthropogenic factors, or arise unforced from the climate system. Distinguishing these factors is essential for estimating sensitivity to multiple climatic forcings and the amplitude of the unforced variability. Here we present 2,000-year-long global mean temperature reconstructions using seven different statistical methods that draw from a global collection of temperature-sensitive palaeoclimate records. Our reconstructions display synchronous multidecadal temperature fluctuations that are coherent with one another and with fully forced millennial model simulations from the Coupled Model Intercomparison Project Phase 5 across the Common Era. A substantial portion of pre-industrial (1300-1800 CE) variability at multidecadal timescales is attributed to volcanic aerosol forcing. Reconstructions and simulations qualitatively agree on the amplitude of the unforced global mean multidecadal temperature variability, thereby increasing confidence in future projections of climate change on these timescales. The largest warming trends at timescales of 20 years and longer occur during the second half of the twentieth century, highlighting the unusual character of the warming in recent decades. |
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| Beschreibung: | Gesehen am 19.09.2019 |
| Beschreibung: | Online Resource |
| ISSN: | 1752-0908 |
| DOI: | 10.1038/s41561-019-0400-0 |