4.7 Article

Medieval Irish chronicles reveal persistent volcanic forcing of severe winter cold events, 431-1649 CE

Journal

ENVIRONMENTAL RESEARCH LETTERS
Volume 8, Issue 2, Pages -

Publisher

IOP Publishing Ltd
DOI: 10.1088/1748-9326/8/2/024035

Keywords

volcano-climate; palaeoclimate; temperature extremes; Ireland; Northeast Atlantic; ice-cores; medieval chronicles

Funding

  1. Ziff Environmental Fellowship from the Harvard University Center for the Environment
  2. Government of Ireland Postgraduate Scholarship from the Irish Research Council for the Humanities and Social Sciences
  3. Irish Environmental Protection Agency's Climate Change Research Programme (CCRP/2.7-Extreme Weather, Climatic Shifts & Natural Disasters in Ireland)
  4. Kernan Brothers Environmental Fellowship from the Harvard University Center for the Environment
  5. National Science Foundation grant [NSF ATM-0902374]
  6. Irish Environmental Protection Agency's Climate Change Research Programme (CCRP/2.7)
  7. Directorate For Geosciences
  8. Div Atmospheric & Geospace Sciences [0902374] Funding Source: National Science Foundation

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Explosive volcanism resulting in stratospheric injection of sulfate aerosol is a major driver of regional to global climatic variability on interannual and longer timescales. However, much of our knowledge of the climatic impact of volcanism derives from the limited number of eruptions that have occurred in the modern period during which meteorological instrumental records are available. We present a uniquely long historical record of severe short-term cold events from Irish chronicles, 431-1649 CE, and test the association between cold event occurrence and explosive volcanism. Thirty eight (79%) of 48 volcanic events identified in the sulfate deposition record of the Greenland Ice Sheet Project 2 ice-core correspond to 37 (54%) of 69 cold events in this 1219 year period. We show this association to be statistically significant at the 99.7% confidence level, revealing both the consistency of response to explosive volcanism for Ireland's climatically sensitive Northeast Atlantic location and the large proportional contribution of volcanism to historic cold event frequencies here. Our results expose, moreover, the extent to which volcanism has impacted winter-season climate for the region, and can help to further resolve the complex spatial patterns of Northern Hemisphere winter-season cooling versus warming after major eruptions.

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