Termination of the Medieval Warm Period: linking sub-polar and tropical N Atlantic circulation changes to ENSO

Research output: Contribution to journalArticleResearch

Abstract

Paleoceanographic evidence from the N Atlantic subpolar gyre and NE Caribbean indicates a major, long-term change in ocean-atmosphere circulation modes around AD 1230, indicating that the termination of the Medieval Warm Period prevailing circulation mode occurred prior to the Wolf Solar Minimum, apparently
without an obvious external trigger.
Original languageEnglish
Pages (from-to)76-77
Number of pages2
JournalPAGES Magazine
Volume17
Issue number2
DOIs
Publication statusPublished - Jun 2009

Programme Area

  • Programme Area 5: Nature and Climate

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