Please use this identifier to cite or link to this item: https://doi.org/10.1088/1748-9326/8/2/024035
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dc.titleMedieval Irish chronicles reveal persistent volcanic forcing of severe winter cold events, 431-1649 CE
dc.contributor.authorLudlow, F
dc.contributor.authorStine, A.R
dc.contributor.authorLeahy, P
dc.contributor.authorMurphy, E
dc.contributor.authorMayewski, P.A
dc.contributor.authorTaylor, D
dc.contributor.authorKillen, J
dc.contributor.authorBaillie, M.G.L
dc.contributor.authorHennessy, M
dc.contributor.authorKiely, G
dc.date.accessioned2020-10-28T07:26:26Z
dc.date.available2020-10-28T07:26:26Z
dc.date.issued2013
dc.identifier.citationLudlow, F, Stine, A.R, Leahy, P, Murphy, E, Mayewski, P.A, Taylor, D, Killen, J, Baillie, M.G.L, Hennessy, M, Kiely, G (2013). Medieval Irish chronicles reveal persistent volcanic forcing of severe winter cold events, 431-1649 CE. Environmental Research Letters 8 (2) : 24035. ScholarBank@NUS Repository. https://doi.org/10.1088/1748-9326/8/2/024035
dc.identifier.issn17489326
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/181833
dc.description.abstractExplosive 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. © 2013 IOP Publishing Ltd.
dc.rightsAttribution 4.0 International
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.sourceUnpaywall 20201031
dc.subjectSubmarine geophysics
dc.subjectice-cores
dc.subjectIreland
dc.subjectmedieval chronicles
dc.subjectNorth East Atlantic
dc.subjectPalaeoclimate
dc.subjectTemperature extremes
dc.subjectvolcano-climate
dc.subjectVolcanoes
dc.subjectaerosol
dc.subjectatmospheric deposition
dc.subjectfrequency analysis
dc.subjectglobal climate
dc.subjectinstrumentation
dc.subjectMedieval
dc.subjectNorthern Hemisphere
dc.subjectpaleoclimate
dc.subjectstratosphere
dc.subjectsulfate
dc.subjecttimescale
dc.subjectvolcanism
dc.subjectArctic
dc.subjectAtlantic Ocean
dc.subjectAtlantic Ocean (Northeast)
dc.subjectGreenland
dc.subjectGreenland Ice Sheet
dc.subjectIreland
dc.typeArticle
dc.contributor.departmentGEOGRAPHY
dc.description.doi10.1088/1748-9326/8/2/024035
dc.description.sourcetitleEnvironmental Research Letters
dc.description.volume8
dc.description.issue2
dc.description.page24035
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