Cooling period in Northern Hemisphere caused by volcanic eruptions From Wikipedia, the free encyclopedia
The volcanic winter of 536 was the most severe and protracted episode of climatic cooling in the Northern Hemisphere in the last 2,000 years.[1] The volcanic winter was caused by at least three simultaneous eruptions of uncertain origin, with several possible locations proposed in various continents. Most contemporary accounts of the volcanic winter are from authors in Constantinople[citation needed], the capital of the Eastern Roman Empire, although the impact of the cooler temperatures extended beyond Europe. Modern scholarship has determined that in early AD 536 (or possibly late 535), an eruption ejected massive amounts of sulfate aerosols into the atmosphere, which reduced the solar radiation reaching the Earth's surface and cooled the atmosphere for several years. In March 536, Constantinople began experiencing darkened skies and lower temperatures.
Tombstone in the chapel of Filippo e Giacomo, Nosedo, dated to AD 536 (the second year after the consulship of Decius Paulinus).
Summer temperatures in 536 fell by as much as 2.5°C (4.5°F) below normal in Europe. The lingering impact of the volcanic winter of 536 was augmented in 539–540, when another volcanic eruption caused summer temperatures to decline as much as 2.7°C (4.9°F) below normal in Europe.[2] There is evidence of still another volcanic eruption in 547 which would have extended the cool period. The volcanic eruptions caused crop failures, and were accompanied by the Plague of Justinian, famine, and millions of deaths and initiated the Late Antique Little Ice Age, which lasted from 536 to 560.[3]
The medieval scholar Michael McCormick wrote that 536 "was the beginning of one of the worst periods to be alive, if not the worst year."[4]
The Roman historian Procopius recorded in AD 536 in his report on the wars with the Vandals, "during this year a most dread portent took place. For the sun gave forth its light without brightness... and it seemed exceedingly like the sun in eclipse, for the beams it shed were not clear".[5][6]
In 538, the Roman statesman Cassiodorus described the following to one of his subordinates in letter 25:[7]
The sun's rays were weak, and they appeared a "bluish" colour.
At noon, no shadows from people were visible on the ground.
The heat from the sun was feeble.
The moon, even when full, was "empty of splendour"
"A winter without storms, a spring without mildness, and a summer without heat"
Prolonged frost and unseasonable drought
The seasons "seem to be all jumbled up together"
The sky is described as "blended with alien elements" just like cloudy weather, except prolonged. It was "stretched like a hide across the sky" and prevented the "true colours" of the sun and moon from being seen, along with the sun's warmth.
Frosts during harvest, which made apples harden and grapes sour.
The need to use stored food to last through the situation.
Subsequent letters (no. 26 and 27) discuss plans to relieve a widespread famine.
In the entry corresponding to the year 535–536, the early 7th century Mandaean Book of Kings relates, "were you to request a tenth of a peck of grain in the land Gawkāy for five staters, we would look but it would not be found,"[8] an exchange of 873 grams of grain for 43 grams of gold, reflecting the scarcity of grain during this time.
In 2015, revision of polar ice core chronologies dated sulfate deposits and a cryptotephra layer to the exact year AD 536 (previously dated to AD 529 before revision).[26] This is strong evidence that a large explosive volcanic eruption caused the observed dimming and cooling, removing the need for an extraterrestrial explanation,[22][26] but an impact event around this time period cannot be ruled out.[27]
The source of volcanic eruption remains to be found but several proposed volcanoes have been rejected:
David Keys suggested the volcano Krakatoa by shifting a cataclysm in AD 416 recorded in Javanese Book of Kings to AD 535.[16] Drilling projects in Sunda Strait ruled out any possibility that an eruption took place during this time period.[30]
Robert Dull and colleagues proposed the large VEI-7, Tierra Blanca Joven (TBJ) eruption of the Ilopango caldera.[31][32] Identification of TBJ tephra in ice cores narrowed the eruption date to AD 429–433.[33]
Christopher Loveluck and his colleagues proposed Icelandic volcanos based on the shards from a Swiss glacier.[4][34][35] However, the cryptotephras dated exactly to AD 536 are geochemically distinct from Icelandic tephra,[36] and the shards in the Swiss glacier have large age uncertainty.[34]
Geochemical analysis of AD 536 cryptotephras distinguishes at least three synchronous eruptive events in North America.[26] Further analysis correlates one of the eruptions to a widespread Mono Craters tephra identified in northeast California.[26][37] The other two eruptions most likely originated from the eastern Aleutians and Northern Cordilleran volcanic province.[26][38]
The 536 event and ensuing famine have been suggested as an explanation for the deposition of hoards of gold by Scandinavian elites at the end of the Migration Period. The gold was possibly a sacrifice to appease the gods and get the sunlight back.[39][40] Mythological events such as the Fimbulwinter and Ragnarök are theorised to be based on the cultural memory of the event.[41]
A book written by David Keys speculates that the climate changes contributed to various developments, such as the emergence of the Plague of Justinian (541–549), the decline of the Avars, the migration of Mongol tribes towards the west, the end of the Sassanid Empire, the collapse of the Gupta Empire, the rise of Islam, the expansion of Turkic tribes, and the fall of Teotihuacán.[16] In 2000, a 3BM Television production (for WNET and Channel Four) capitalised upon Keys' book. The documentary, under the name Catastrophe! How the World Changed, was broadcast in the US as part of PBS's Secrets of the Dead series.[42]
However, Keys and Wohletz's ideas lack mainstream acceptance. Reviewing Keys' book, British archaeologist Ken Dark commented that "much of the apparent evidence presented in the book is highly debatable, based on poor sources or simply incorrect. [...] Nonetheless, both the global scope and the emphasis on the 6th century AD as a time of wide-ranging change are notable, and the book contains some obscure information that will be new to many. However, it fails to demonstrate its central thesis and does not offer a convincing explanation for the many changes discussed".[43]
The philologist Andrew Breeze in a recent book (2020) argues that some Arthurian events, including the Battle of Camlann, are historical, happening in 537 as a consequence of the famine associated with the climate change of the previous year.[44]
Historian Robert Bruton argues that this catastrophe played a role in the decline of the Roman Empire.[45]
Abbott, D. H.; Biscaye, P.; Cole-Dai, J.; Breger, D. (December 2008). "Magnetite and Silicate Spherules from the GISP2 Core at the 536 A.D. Horizon". AGU Fall Meeting Abstracts. American Geophysical Union, Fall Meeting 2008. Vol.41. pp.41B–1454. Bibcode:2008AGUFMPP41B1454A. Abstract #PP41B-1454.
Procopius (1916). Procopius. Vol.2: History of the [Vandalic] Wars, Books III and IV. Translated by Dewing, Henry Bronson. London, England: William Heinemann. p.329. ISBN978-0-674-99054-8.
Ochoa, George; Hoffman, Jennifer; Tin, Tina (2005). Climate: the force that shapes our world and the future of life on earth. Emmaus, Pennsylvania: Rodale. ISBN978-1-59486-288-5, gives this quote as "The Sun gave forth its light without brightness, like the moon during this whole year, and it seemed exceedingly like the Sun in eclipse".
Cassiodorus (1886). The Letters of Cassiodorus. Translated by Hodgkin, Thomas. London, England: Henry Frowde. pp.518–520. See: "25. Senator, Praetorian Praefect, to his deputy Ambrosius, an Illustris."
Michel le Syrien (1901). Chronique de Michel le Syrien, Patriarche Jacobite d'Antoche[Chronicle of Michael the Syrian, Jacobite Patriarch of Syria] (in French). Vol.2. Translated by Chabot, J. -B. Paris, France: Leroux. pp.220–221. "Or, un peu auparavant, en l'an 848, il y eut un signe dans le soleil..., et le vin avait le goût de celui qui provient de raisins acides." (However, a little earlier, in the year 848 [according to the Greek calendar; AD 536/537 according to the Christian calendar], there was a sign in the sun. One had never seen it [before] and nowhere is it written that such [an event] had happened [previously] in the world. If it were not [true] that we found it recorded in most proven and credible writings, and confirmed by men worthy of belief, we would not have written it [here]; for it's difficult to conceive. So it is said that the sun was darkened and that its eclipse lasted a year and a half, that is, eighteen months. Every day it shone for about four hours and yet this light was only a feeble shadow. Everyone declared that it would not return to the state of its original light. Fruits did not ripen, and wine had the taste of what comes from sour grapes.)
Ochoa, George; Hoffman, Jennifer; Tin, Tina (2005). Climate: the force that shapes our world and the future of life on earth. Emmaus, Pennsylvania: Rodale. p.71. ISBN978-1-59486-288-5.
Stothers, R. B.; Rampino, M. R. (1983). "Volcanic eruptions in the Mediterranean before AD 630 from written and archaeological sources". Journal of Geophysical Research. 88 (B8): 6357–6471. Bibcode:1983JGR....88.6357S. doi:10.1029/JB088iB08p06357. ISSN0148-0227.
Dull, R.; Southon, J. R.; Kutterolf, S.; Freundt, A.; Wahl, D.; Sheets, P. (13–17 December 2010). "Did the TBJ Ilopango eruption cause the AD 536 event?". AGU Fall Meeting Abstracts. 13: V13C–2370. Bibcode:2010AGUFM.V13C2370D.
Ström, Folke: Nordisk Hedendom, Studentlitteratur, Lund 2005, ISBN91-44-00551-2 (first published 1961) among others, refer to the climate change theory.
Gunn, Joel D. (2000). The Years Without Summer: Tracing A.D. 536 and its Aftermath. British Archaeological Reports (BAR) International. Oxford, England: Archaeopress. ISBN978-1-84171-074-7.
Arjava, Antti (2006). "The Mystery Cloud of 536 CE in the Mediterranean Sources". Dumbarton Oaks Papers. Vol.59. Washington, DC: Dumbarton Oaks Research Library and Collection. pp.73–94.
Axboe, Morten (2001). "Amulet Pendants and a Darkened Sun". In Bente Magnus (ed.). Roman Gold and the Development of the Early Germanic Kingdoms: Aspects of Technical, Socio-political, Socio-economic, Artistic and Intellectual Development, A.D. 1–500. Almquiest & Wiksell Intl. p.51. ISBN978-91-7402-310-7.
Gunn, Joel (2000). The Years Without Summer: Tracing A.D. 536 and its Aftermath. British Archaeological Reports (BAR) International. Oxford, England: Archaeopress. ISBN978-1-84171-074-7.