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.
without an obvious external trigger.
| Original language | English |
|---|---|
| Pages (from-to) | 76-77 |
| Number of pages | 2 |
| Journal | PAGES Magazine |
| Volume | 17 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - Jun 2009 |
Programme Area
- Programme Area 5: Nature and Climate
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