http://www.nature.com/nature/journal/v523/n7562/full/nature14565.html

Timing and climate forcing of volcanic eruptions for the past 2,500 years

M. Sigl,         M. Winstrup,    J. R. McConnell,        K. C. Welten,   G. 
Plunkett,    F. Ludlow,      U. Büntgen,     M. Caffee,      N. Chellman,    D. 
Dahl-Jensen,         H. Fischer,     S. Kipfstuhl,   C. Kostick,     O. J. 
Maselli,  F. Mekhaldi,    R. Mulvaney,    R. Muscheler,   D. R. Pasteris,       
  J. R. Pilcher,  M. Salzer,      S. Schüpbach, J. P. Steffensen,         B. M. 
Vinther   & T. E. Woodruff
AffiliationsContributionsCorresponding author
Nature 523, 543–549 (30 July 2015) doi:10.1038/nature14565

Abstract
Volcanic eruptions contribute to climate variability, but quantifying these 
contributions has been limited by inconsistencies in the timing of atmospheric 
volcanic aerosol loading determined from ice cores and subsequent cooling from 
climate proxies such as tree rings. Here we resolve these inconsistencies and 
show that large eruptions in the tropics and high latitudes were primary 
drivers of interannual-to-decadal temperature variability in the Northern 
Hemisphere during the past 2,500 years. Our results are based on new records of 
atmospheric aerosol loading developed from high-resolution, multi-parameter 
measurements from an array of Greenland and Antarctic ice cores as well as 
distinctive age markers to constrain chronologies. Overall, cooling was 
proportional to the magnitude of volcanic forcing and persisted for up to ten 
years after some of the largest eruptive episodes. Our revised timescale more 
firmly implicates volcanic eruptions as catalysts
 in the major sixth-century pandemics, famines, and socioeconomic disruptions 
in Eurasia and Mesoamerica while allowing multi-millennium quantification of 
climate response to volcanic forcing.

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