http://onlinelibrary.wiley.com/doi/10.1002/jgrd.50513/abstract

Cool North European summers and possible links to explosive volcanic
eruptions

P. D Jones, T. M. Melvin, C. Harpham1, H. Grudd, S. Helama
DOI: 10.1002/jgrd.50513
Journal of Geophysical Research: Atmospheres
Volume 118, Issue 12, pages 6259–6265, 27 June 2013

Abstract
Exactly dated tree-ring measurements such as ring width (TRW) and maximum
latewood density (MXD), which are sensitive to summer temperatures, can
provide possible routes to investigate the occurrence of hemispheric-wide
cool summers that might be linked to explosive tropical volcanic eruptions.
These measurements can provide much longer records than the instrumental
period, enabling much longer periods to be assessed and offers the
potential to look at much larger eruptions than recorded over the last 200
years. This paper looks at TRW evidence from Northern Fennoscandia
extending over the last 7500 years, using two independently produced
chronologies from northern Sweden and northern Finland. TRW is less
responsive than MXD to cool summer temperatures, but MXD is only available
for the last 2000 years. Additionally, looking at a relatively small
location, compared to the Northern Hemisphere average, adds considerable
noise. Progress in this area is likely to be made by developing more
millennial-long TRW series across northern high latitudes or being able to
develop MXD series from the sub-fossil material, which comprises most of
the samples prior to the last 1000 years. The three most extreme negative
values for the region for the last 2000 years are 1601, 542, and 1837,
although the latter is not extreme in a long instrumental record for the
region. The most extreme year of all occurred in 330BC. Of the 20 most
extreme negative years, nine occurred during the AD years with the
remaining 11 occurring during the prior 5500 years.

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