Aerosol size confines climate response to volcanic super-eruptions
Version of Record online: 22 DEC 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 24, December 2010
How to Cite
2010), Aerosol size confines climate response to volcanic super-eruptions, Geophys. Res. Lett., 37, L24705, doi:10.1029/2010GL045464., , , , , , , and (
- Issue online: 22 DEC 2010
- Version of Record online: 22 DEC 2010
- Manuscript Accepted: 9 NOV 2010
- Manuscript Revised: 29 OCT 2010
- Manuscript Received: 13 SEP 2010
Auxiliary material for this article contains additional information about the model and the experimental set up we used for model simulations of the Young Toba tuff eruption and four figures.
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Additional file information is provided in the readme.txt.
|grl27603-sup-0001-readme.txt||plain text document||2K||readme.txt|
|grl27603-sup-0002-txts01.pdf||PDF document||42K||Text S1. Details on model and experimental set up and on statistical significance.|
|grl27603-sup-0003-fs01.eps||PS document||18K||Figure S1. Nino3.4 sea surface temperature anomaly index for the five individual ensemble runs.|
|grl27603-sup-0004-fs02.eps||PS document||4408K||Figure S2. Temperature anomalies (K) for the 1st summer after the eruption for the individual ensembles and the ensemble mean.|
|grl27603-sup-0005-fs03.eps||PS document||4295K||Figure S3. Temperature anomalies (K) for the 2nd winter after the eruption for the individual ensembles and the ensemble mean.|
|grl27603-sup-0006-fs04.eps||PS document||2613K||Figure S4. Temperature and precipitation anomalies for the 1st summer and 2nd winter after the eruption.|
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