Year Without a Summer

Year Without a Summer
1816 summer temperature anomaly compared with average temperatures from 1971 to 2000
VolcanoMount Tambora
Start dateEruption occurred on 10 April 1815
TypeUltra-Plinian
LocationLesser Sunda Islands, Dutch East Indies (now Republic of Indonesia)
ImpactCaused a volcanic winter that dropped temperatures by 0.4–0.7°C (or 0.7–1°F) worldwide

1816 is known as the Year Without a Summer because of severe climate abnormalities that caused average global temperatures to decrease by 0.4–0.7 °C (0.7–1 °F).[1] Summer temperatures in Europe were the coldest of any on record between 1766 and 2000,[2] resulting in crop failures and major food shortages across the Northern Hemisphere.[3]

Evidence suggests that the anomaly was predominantly a volcanic winter event caused by the massive 1815 eruption of Mount Tambora in April in modern-day Indonesia (commonly referred to as the Dutch East Indies at the time). This eruption was the largest in at least 1,300 years (after the hypothesized eruption causing the volcanic winter of 536); its effect on the climate may have been exacerbated by the 1814 eruption of Mayon in the Philippines. The significant amount of volcanic ash and gases released into the atmosphere blocked sunlight, leading to global cooling.

Countries such as Great Britain, Ireland, and France experienced significant hardship, with food riots and famine becoming common. The situation was exacerbated by the fact that Europe was still recovering from the Napoleonic Wars, adding to the socio-economic stress.

North America also faced extreme weather conditions. In the eastern United States, a persistent "dry fog" dimmed the sunlight, causing unusual cold and frost throughout the summer months. Crops failed in regions like New England, leading to food shortages and economic distress. These conditions forced many families to leave their homes in search of better farming opportunities, contributing to Westward expansion.

  1. ^ Stothers, Richard B. (1984). "The Great Tambora Eruption in 1815 and Its Aftermath". Science. 224 (4654): 1191–1198. Bibcode:1984Sci...224.1191S. doi:10.1126/science.224.4654.1191. PMID 17819476. S2CID 23649251.
  2. ^ Schurer, Andrew P.; Hegerl, Gabriele C.; Luterbacher, Jürg; Brönnimann, Stefan; Cowan, Tim; Tett, Simon F. B.; Zanchettin, Davide; Timmreck, Claudia (September 17, 2019). "Disentangling the causes of the 1816 European year without a summer". Environmental Research Letters. 14 (9): 094019. Bibcode:2019ERL....14i4019S. doi:10.1088/1748-9326/ab3a10. hdl:21.11116/0000-0004-B878-6. ISSN 1748-9326.
  3. ^ "Saint John New Brunswick Time Date". New-brunswick.net. Archived from the original on January 9, 2017. Retrieved March 5, 2012.