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|Title:||Massive atmospheric sulfur loading of the AD 1600 Huaynaputina eruption and implications for petrologic sulfur estimates||Authors:||Costa, Fidel
|Keywords:||DRNTU::Science::Geology||Issue Date:||2003||Source:||Costa, F., Scaillet, B., & Gourgaud, A, (2003). Massive atmospheric sulfur loading of the AD 1600 Huaynaputina eruption and implications for petrologic sulfur estimates. Geophysical Research Letters, 30(2).||Series/Report no.:||Geophysical research letters||Abstract:||We combine petrological, analytical, and thermodynamical data to constrain the sulfur yield of the AD 1600 Huaynaputina eruption which has been associated with the largest Earth's temperature shift in the last 600 years. The calculated amount of S (26-55 Tg), partly overlaps, but ranges to almost twice the amount estimated from ice-core data (16-32 Tg), the higher values of our estimate probably reflect that not all S released by the eruption reached the stratosphere. Our study also shows that it is possible to estimate the atmospheric sulfur loading from the volcanic products themselves, which opens the possibility to explore volcano-climate links beyond the time period covered by ice-core archives.||URI:||https://hdl.handle.net/10356/95266
|DOI:||http://dx.doi.org/10.1029/2002GL016402||Rights:||© 2003 American Geophysical Union.This paper was published in Geophysical Research Letters and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The paper can be found at the following official URL: http://dx.doi.org/10.1029/2002GL016402. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law."||Fulltext Permission:||open||Fulltext Availability:||With Fulltext|
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