Image:Greenland sulfate.png

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Description

Sulfate concentration in ice core from Central Greenland, accurately dated by counting oxygen isotope seasonal variations. The year 1815 AD was due to the Mt. Tambora eruption, while prior to that is an unknown eruption.
Source

Dai (1991)[1]
Date

18 October 2006
Author

myself
Permission
(Reusing this image)
GNU head Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation license, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled "GNU Free Documentation license".

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[edit] References

  1. ↑ Dai, J., E. Mosley-Thompson, and L.G. Thompson, 1991. Ice core evidence for an explosive tropical volcanic eruption six years preceding Tambora, Journal of Geophysical Research (Atmospheres), 96, pp. 17,361-17,366.

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current12:45, 18 October 2006394×557 (23 KB)Indon ({{Information |Description= Sulfate concentration in ice core from Central Greenland, accurately dated by counting oxygen isotope seasonal variations. The year 1815 AD was due to the Mt. Tambora eruption, while prior to that is an unkn)
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