articleScienceApr 2, 2009Closed access

Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly

Oeschger Centre for Climate Change Research · Scripps Institution of Oceanography · +3 more institutions

PubMed
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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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Authors

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Topics & keywords

Keywords
  • Atlantic multidecadal oscillation
  • Proxy (statistics)
  • Climatology
  • North Atlantic oscillation
  • Anomaly (physics)
  • General Circulation Model
  • Little ice age
  • Geology
UN Sustainable Development Goals
  • Climate action
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