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Cold decade (AD 1810–1819) caused by Tambora (1815) and another (1809) stratospheric volcanic eruption
Jihong Cole-Dai, David A Ferris, Alyson Lanciki, Joel Savarino, Mélanie Baroni, Mark H Thiemens

Cold decade (AD 1810–1819) caused by Tambora (1815) and another (1809) stratospheric volcanic eruption

Science & Mathematics Published 2009 Verification Pending

Overview & Synopsis

Climate records indicate that the decade of AD 1810–1819 including “the year without a summer” (1816) is probably the coldest during the past 500 years or longer, and the cause of the climatic extreme has been attributed primarily to the 1815 cataclysmic Tambora eruption in Indonesia. But the cold temperatures in the early part of the decade and the timing of the Tambora eruption call into question the real climatic impact of volcanic eruptions. Here we present new evidence, based on sulfur isotope anomaly (Δ33S), a unique indicator of volcanic sulfuric acid produced in the stratosphere and preserved in polar snow, and on the precise timing of the volcanic deposition in both polar regions, that another large eruption in 1809 of a volcano is also stratospheric and occurred in the tropics. The Tambora eruption and the undocumented 1809 eruption are together responsible for the unusually cold decade.

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Document Information

Document Title Cold decade (AD 1810–1819) caused by Tambora (1815) and another (1809) stratospheric volcanic eruption
Author / Organization Jihong Cole-Dai, David A Ferris, Alyson Lanciki, Joel Savarino, Mélanie Baroni, Mark H Thiemens
Subject & Discipline Multidisciplinary Academic Open Research
Categories Science & Mathematics
Publication Year 2009
License / Rights Open Access / Creative Commons
Resource Verification Listed PDF (Verification Pending)
Original Host Website HAL Open Science (hal.science)
File Format application/pdf (Portable Document Format)
Language EN
Catalog ID DOC-111896
Original Source Link Visit Source Page on hal.science »