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

Jihong Cole-Dai (1) , David A Ferris (1) , Alyson Lanciki (1) , Joel Savarino (2) , Mélanie Baroni (3) , Mark H Thiemens (4)

1 Department of Chemistry and Biochemistry [Brookings]
2 LGGE - Laboratoire de glaciologie et géophysique de l'environnement
3 CEREGE - Centre européen de recherche et d'enseignement des géosciences de l'environnement
4 Department of Chemistry and Biochemistry

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.

Domaines: Climatologie; Volcanologie

Jihong Cole-Dai, David A Ferris, Alyson Lanciki, Joel Savarino, Mélanie Baroni, et al.. Cold decade (AD 1810–1819) caused by Tambora (1815) and another (1809) stratospheric volcanic eruption. Geophysical Research Letters, 2009, 36 (22), pp.L22703. ⟨10.1029/2009GL040882⟩. ⟨hal-01757253⟩