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Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly
Abstract
The Medieval Climate Anomaly (MCA) was the most recent pre-industrial era warm interval of European climate, yet its driving mechanisms remain uncertain. We present here a 947-year-long multidecadal North Atlantic Oscillation (NAO) reconstruction and find a persistent positive NAO during the MCA. Supplementary reconstructions based on climate model results and proxy data indicate a clear shift to weaker NAO conditions into the Little Ice Age (LIA). Globally distributed proxy data suggest that this NAO shift is one aspect of a global MCA-LIA climate transition that probably was coupled to prevailing La Niña–like conditions amplified by an intensified Atlantic meridional overturning circulation during the MCA.
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Mangini, A., Spötl, C., & Verdes, P. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.05.010 · Cited by 294
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Metadata
- Authors
- Trouet, V., Esper, J., Graham, N. E., Baker, A., Scourse, J. D., & Frank, D. C.
- Venue
- Science
- Published
- 2009-04-03
- Volume
- 324
- Issue
- 5923
- Pages
- 78-80
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2034795620
- Cited by
- 1,073
- References
- 1
- FWCI
- 49.22
- Type
- journal article
- Language
- en
- Open access
- closed
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- Trouet, V., Esper, J., Graham, N. E., Baker, A., Scourse, J. D., & Frank, D. C. (2009). Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly. Science. https://doi.org/10.1126/science.1166349
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