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The 1452/1453 mystery eruption is an unidentified volcanic event that triggered the first large sulfate spike in the 1450s, succeeded by another spike in 1458 caused by another mysterious eruption. The eruption caused a severe volcanic winter leading to one of strongest cooling events in the Northern Hemisphere.
Jun 27, 2006 · Our results suggest that the Kuwae eruption is a single-phase eruption which took place in late 1452 or early 1453, producing significant depositions that lasted up to four years in both Greenland and Antarctic ice sheets.
- Chaochao Gao, Alan Robock, Stephen Self, Jeffrey B. Witter, J. P. Steffenson, Henrik Brink Clausen, ...
- 2006
The 1452 or 1453 A.D. Kuwae Eruption Signal Derived from Multiple Ice Core Records: Greatest Volcanic Sulfate Event of the Past 700 Years Chaochao Gao1, Alan Robock1, Stephen Self2, Jeffrey B.Witter3, J. P. Steffenson4, Henrik Brink Clausen4, Marie-Louise Siggaard-Andersen4, Sigfus Johnsen4, Paul A. Mayewski5, and Caspar Ammann6
The 1452 or 1453 A.D. Kuwae eruption signal derived from multiple ice core records: Greatest volcanic sulfate event of the past 700 years. Publication Title. Journal of Geophysical Research-Atmospheres. Date. 2006-06-27. Volume. 111. Issue. D12. Article Number. D12107. Resource Type. article. Peer Review. Refereed. Copyright Information.
Jun 27, 2006 · The 1452 or 1453 A.D. Kuwae eruption signal derived from multiple ice core records : Greatest volcanic sulfate event of the past 700 years. Chaochao Gao, A. Robock, +7 authors. C. Ammann. Published 27 June 2006. Environmental Science, Geology. Journal of Geophysical Research.
The 1452 or 1453 A.D. Kuwae eruption signal derived from multiple ice core records: Greatest volcanic sulfate event of the past 700 years - Gao - 2006 - Journal of Geophysical Research: Atmospheres - Wiley Online Library.
The results suggest only one major stratospheric injection from the Kuwae eruption and confirm previous findings that the Kuwae eruption took place in late 1452 or early 1453, which may serve as a reference to evaluate and improve the dating of ice core records.
