http://onlinelibrary.wiley.com/doi/10.1029/2012JD018603/abstract

Sigl, M., et al. (2013), A new bipolar ice core record of volcanism from
WAIS Divide and NEEM and implications for climate forcing of the last 2000
years, J. Geophys. Res. Atmos., 118, 1151–1169, doi:10.1029/2012JD018603

Keywords:

ice cores;volcanic forcing;Kuwae;Taupo;explosive volcanism;WAIS timescale

Abstract

Volcanism is a natural climate forcing causing short-term variations in
temperatures. Histories of volcanic eruptions are needed to quantify their
role in climate variability and assess human impacts. We present two new
seasonally resolved, annually dated non-sea-salt sulfur records from polar
ice cores—WAIS Divide (WDC06A) from West Antarctica spanning 408 B.C.E. to
2003 C.E. and NEEM (NEEM-2011-S1) from Greenland spanning 78 to 1997
C.E.—both analyzed using high-resolution continuous flow analysis coupled
to two mass spectrometers. The high dating accuracy allowed placing the
large bi-hemispheric deposition event ascribed to the eruption of Kuwae in
Vanuatu (previously thought to be 1452/1453 C.E. and used as a tie-point in
ice core dating) into the year 1458/1459 C.E. This new age is consistent
with an independent ice core timescale from Law Dome and explains an
apparent delayed response in tree rings to this volcanic event. A second
volcanic event is detected in 1453 C.E. in both ice cores. We show for the
first time ice core signals in Greenland and Antarctica from the strong
eruption of Taupo in New Zealand in 232 C.E. In total, 133 volcanic events
were extracted from WDC06A and 138 from NEEM-2011-S1, with 50 ice core
signals—predominantly from tropical source volcanoes—identified
simultaneously in both records. We assess the effect of large bipolar
events on temperature-sensitive tree ring proxies. These two new volcanic
records, synchronized with available ice core records to account for
spatial variability in sulfate deposition, provide a basis for improving
existing time series of volcanic forcing.

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