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

Antoon Kuijpers; B.A. Malmgren; M.-S. Seidenkrantz

doi:10.22498/pages.17.2.76

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

Antoon Kuijpers, B.A. Malmgren, M.-S. Seidenkrantz

Overfladenær Land- og Maringeologi

Publikation: Bidrag til tidsskrift › Artikel › Forskning

Resumé

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.

Originalsprog	Engelsk
Sider (fra-til)	76-77
Antal sider	2
Tidsskrift	PAGES Magazine
Vol/bind	17
Udgave nummer	2
DOI	https://doi.org/10.22498/pages.17.2.76
Status	Udgivet - jun. 2009

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Programområde 5: Natur og klima

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10.22498/pages.17.2.76Licens: CC BY

Citationsformater

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

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, apparentlywithout an obvious external trigger.",

author = "Antoon Kuijpers and B.A. Malmgren and M.-S. Seidenkrantz",

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AB - 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, apparentlywithout an obvious external trigger.

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DO - 10.22498/pages.17.2.76

M3 - Article

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

Resumé

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