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New ice core evidence for a volcanic cause of the A.D. 536 dust veil

Larsen, LB (author)
Vinther, BM (author)
Briffa, KR (author)
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Melvin, TM (author)
Clausen, HB (author)
Jones, PD (author)
Siggaard-Andersen, M-L (author)
Hammer, CU (author)
Eronen, M (author)
Grudd, H (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Gunnarson, BE (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Hantemirov, RM (author)
Naurzbaev, MM (author)
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 (creator_code:org_t)
2008
2008
English.
In: Geophysical Research Letters. ; 35:L04708
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • New and well-dated evidence of sulphate deposits in Greenland and Antarctic ice cores indicate a substantial and extensive atmospheric acidic dust veil at A.D. 533–534 ± 2 years. This was likely produced by a large explosive, near equatorial volcanic eruption, causing widespread dimming and contributing to the abrupt cooling across much of the Northern Hemisphere known from historical records and tree-ring data to have occurred in A.D. 536. Tree-ring data suggest that this was the most severe and protracted short-term cold episode across the Northern Hemisphere in the last two millennia, even surpassing the severity of the cold period following the Tambora eruption in 1815.

Keyword

A.D. 536 cooling; volcanism; climate

Publication and Content Type

ref (subject category)
art (subject category)

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