http://onlinelibrary.wiley.com/doi/10.1029/2012GL054246/abstract

Xu, J., B. Pan, T. Liu, I. Hajdas, B. Zhao, H. Yu, R. Liu, and P.
Zhao (2013), Climatic impact of the Millennium eruption of Changbaishan
volcano in China: New insights from high-precision radiocarbon wiggle-match
dating, Geophys. Res. Lett., 40, 54–59, doi:10.1029/2012GL054246.

Abstract

Changbaishan volcano in northeast China, previously dated to have erupted
around the mid-10th century A.D., is renowned for producing one of the
largest eruptions in history (magnitude 6.8) and thus speculated to have
substantial climatic impact. Here we report a new high-precision 14C
wiggle-match age of A.D. 946 ± 3 obtained from a 264 year old tree trunk
(with bark) killed during the eruption, using the OxCal's Bayesian modeling
approach with 27 sequentially sampled annual rings of decadal intervals.
The new chronology conforms well to the calendar date of A.D. 946 for the
eruption inferred from historical documentary evidence. We find no
stratospherically loaded sulfate spike that might be associated with the
A.D. 946 eruption in the global volcanism record from the GISP2 ice core,
suggesting the stratospheric sulfate aerosols produced during the eruption
were not transported to the arctic region, due probably to its relatively
low stratospheric sulfur emission and the seasonal effects of the
atmospheric circulation at the time of the eruption that likely occurred in
the winter of A.D. 946–947. Since the stratospheric volcanic sulfates are
the main cause of large-scale climate perturbations, this finding indicates
that the Millennium eruption of Changbaishan volcano might have limited
regional climatic effects, rather than global or hemispheric impact as
implied by its magnitude.

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