Poster's note : this is a really informative study, and I look forward to
other researchers building on it. Especially fruitful may be a study of
cause of death from dated graves, allowing a history of conflict and
starvation to be tied to the eruption history. It also perhaps serves as a
cautionary note to proposals for monohemispheric injection proposals.

http://onlinelibrary.wiley.com/doi/10.1002/2013JD021061/abstract

Proxy evidence for China's monsoon precipitation response to volcanic
aerosols over the past seven centuries

Zhihong Zhuo1, Chaochao Gao1,*andYuqing Pan2

Article first published online: 3 JUN 2014

DOI: 10.1002/2013JD021061

Journal of Geophysical Research: Atmospheres

Volume 119, Issue 11, pages 6638–6652, 16 June 2014

Keywords:

volcanic eruption;monsoon precipitation;

Abstract

The effect of volcanic aerosols on China's monsoon precipitation over the
past 700 years has been studied using two independently compiled histories
of volcanism combined with the Monsoon Asia Drought Atlas. For both
reconstructions, four categories of eruptions are distinguished based on
the character of their Northern Hemisphere (NH) injection; then Superposed
Epoch Analysis (SEA) with a 10,000 Monte Carlo resampling procedure is
undertaken for each category and also each individual grid. Results show a
statistically significant (at 90% confidence level) drying trend over
mainland China from year 1 to year 4 after the eruptions, and the more
sulfate aerosol that is injected into the NH stratosphere, the more severe
this drying trend. In comparison, a minor wetting trend is observed in the
years following Southern Hemisphere-only injections. Results from spatial
distribution of the SEA show (1) a southward movement of the significant
dry areas in eastern China from year 0 to year 2 after volcanic
perturbations that are either equal to or double the size of the 1991 Mount
Pinatubo eruption (15 T sulfate aerosols in NH) and (2) northeast and
northwest China experienced substantial droughts in years 2 to 5. These
results are in good agreement with a SEA analysis of the Chinese Historical
Drought Disaster Index compiled from historical meteorological records. Our
findings illustrate the important role stratospheric aerosols have played
in altering China's precipitation during the summer monsoon season and can
shed new light on the possible effects that stratospheric geoengineering
may have on China's precipitation.

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