Timing and climate forcing of volcanic eruptions for the past 2,500 years
Language English Country Great Britain, England Media print-electronic
Document type Historical Article, Journal Article, Research Support, Non-U.S. Gov't, Research Support, U.S. Gov't, Non-P.H.S.
PubMed
26153860
DOI
10.1038/nature14565
PII: nature14565
Knihovny.cz E-resources
- MeSH
- Aerosols analysis MeSH
- Atmosphere chemistry MeSH
- Beryllium MeSH
- Time Factors MeSH
- History, Ancient MeSH
- History, Medieval MeSH
- Disasters history MeSH
- Ice analysis MeSH
- Climate * MeSH
- Radiometric Dating MeSH
- Carbon Radioisotopes MeSH
- Radioisotopes MeSH
- Seasons MeSH
- Sulfur MeSH
- Volcanic Eruptions history MeSH
- Trees anatomy & histology growth & development MeSH
- Temperature * MeSH
- Tropical Climate MeSH
- Check Tag
- History, Ancient MeSH
- History, Medieval MeSH
- Publication type
- Journal Article MeSH
- Historical Article MeSH
- Research Support, Non-U.S. Gov't MeSH
- Research Support, U.S. Gov't, Non-P.H.S. MeSH
- Geographicals
- Americas MeSH
- Antarctic Regions MeSH
- Europe MeSH
- Greenland MeSH
- Names of Substances
- Aerosols MeSH
- Beryllium MeSH
- Ice MeSH
- Carbon Radioisotopes MeSH
- Radioisotopes MeSH
- Sulfur MeSH
Volcanic eruptions contribute to climate variability, but quantifying these contributions has been limited by inconsistencies in the timing of atmospheric volcanic aerosol loading determined from ice cores and subsequent cooling from climate proxies such as tree rings. Here we resolve these inconsistencies and show that large eruptions in the tropics and high latitudes were primary drivers of interannual-to-decadal temperature variability in the Northern Hemisphere during the past 2,500 years. Our results are based on new records of atmospheric aerosol loading developed from high-resolution, multi-parameter measurements from an array of Greenland and Antarctic ice cores as well as distinctive age markers to constrain chronologies. Overall, cooling was proportional to the magnitude of volcanic forcing and persisted for up to ten years after some of the largest eruptive episodes. Our revised timescale more firmly implicates volcanic eruptions as catalysts in the major sixth-century pandemics, famines, and socioeconomic disruptions in Eurasia and Mesoamerica while allowing multi-millennium quantification of climate response to volcanic forcing.
Alfred Wegener Institut Helmholtz Zentrum für Polar und Meeresforschung 27570 Bremerhaven Germany
British Antarctic Survey Natural Environment Research Council Cambridge CB3 0ET UK
Centre for Ice and Climate Niels Bohr Institute University of Copenhagen 2100 Copenhagen Denmark
Department of Earth and Space Sciences University of Washington Seattle Washington 98195 USA
Department of Geology Quaternary Sciences Lund University 22362 Lund Sweden
Department of History The University of Nottingham Nottingham NG7 2RD UK
Department of Physics Purdue University West Lafayette Indiana 47907 USA
Desert Research Institute Nevada System of Higher Education Reno Nevada 89512 USA
School of Geography Archaeology and Palaeoecology Queen's University Belfast Belfast BT7 1NN UK
Space Sciences Laboratory University of California Berkeley California 94720 USA
The Laboratory of Tree Ring Research University of Arizona Tucson Arizona 85721 USA
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