The Dust Veil Environmental Disaster of AD 536

According to written records and supported by dendrochronology (tree ring) and archaeological evidence, for 12-18 months in AD 536-537, a thick, persistent dust veil or dry fog darkened the skies between Europe and Asia Minor. The climatic interruption brought by the thick, bluish fog extended as far east as China, where summer frosts and snow are mentioned in historical records; tree ring data from Mongolia and Siberia to Argentina and Chile reflect decreased growing records from 536 and the subsequent decade. The climatic effects of the dust veil brought decreased temperatures, drought, and food shortages throughout the affected regions: in Europe, two years later came the Justinian plague. The combination killed perhaps as much as 1/3 of the population of Europe; in China, the famine killed perhaps 80% of people in some regions; and in Scandinavia, the losses may have been as much as 75-90% of the population, as evidenced by the numbers of deserted villages and cemeteries. Historical Documentation The rediscovery of the AD 536 event was made during the 1980s by American geoscientists Stothers and Rampino, who searched classical sources for evidence of volcanic eruptions. Among their other findings, they noted several references to environmental disasters around the world between AD 536-538. Contemporary reports identified by Stothers and Rampino included Michael the Syrian, who wrote: [T]he sun became dark and its darkness lasted for one and a half years [...] Each day it shone for about four hours and still this light was only a feeble shadow [...] the fruits did not ripen and the wine tasted like sour grapes. John of Ephesus related much the same events. Prokopios, who lived in both Africa and Italy at the time, said: For the sun gave forth its light without brightness, like the moon, during this whole year, and it seemed exceedingly like the sun in eclipse, for the beams it shed were not clear nor such as it is accustomed to shed. An anonymous Syrian chronicler wrote: [T]he sun began to be darkened by day and the moon by night, while the ocean was tumultuous with spray, from the 24th of March in this year till the 24th of June in the following year... The following winter in Mesopotamia was so bad that from the large and unwonted quantity of snow the birds perished. A Summer Without Heat Cassiodorus, praetorian prefect of Italy at the time, wrote: so we have had a winter without storms, spring without mildness, summer without heat. John Lydos, in On Portents, writing from Constantinople, said: If the sun becomes dim because the air is dense from rising moisture—as happened in [536/537] for nearly a whole year [...] so that produce was destroyed because of the bad time—it predicts heavy trouble in Europe. In China, reports indicate that the star of Canopus could not be seen in as usual in the spring and fall equinoxes of 536, and the years AD 536-538 were marked by summer snows and frosts, drought and severe famine. In some parts of China, the weather was so severe that 70-80% of the people starved to death. Physical Evidence Tree rings show that 536 and the following ten years was a period of slow growth for Scandinavian pines, European oaks and even several North American species including bristlecone pine and foxtail; similar patterns of ring size decrease are also seen in trees in Mongolia and northern Siberia. But there seems to be something of a regional variation in the worst of the effects. 536 was a bad growing season in many parts of the world, but more generally, it was a part of a decade-long downturn in climate for the northern hemisphere, separate from the worst seasons by 3-7 years. For most reports in Europe and Eurasia, there is a drop in 536, followed by a recovery in 537-539, followed by a more serious plunge lasting perhaps as late as 550. In most cases the worst year for tree ring growth is 540; in Siberia 543, southern Chile 540, Argentina 540-548. AD 536 and the Viking Diaspora Archaeological evidence described by Grà ¤slund and Price shows that Scandinavia might have experienced the worst troubles. Almost 75% of villages were abandoned in parts of Sweden, and areas of southern Norway show a decrease in formal burials—indicating that haste was required in interments—up to 90-95%. Scandinavian narratives recount possible events that might be referring to 536. Snorri Sturlusons Edda includes a reference to Fimbulwinter, the great or mighty winter that served as a forewarning of Ragnarà ¶k, the destruction of the world and all of its inhabitants. First of all that a winter will come called Fimbulwinter. Then snow will drift from all directions. There will then be great frosts and keen winds. The sun will do no good. There will be three of these winters together and no summer between. Grà ¤slund and Price speculate that the social unrest and sharp agrarian decline and demographic disaster in Scandinavia may have been a primary catalyst for the Viking diaspora—when in the 9th century AD, young men left Scandinavia in droves  and sought to conquer new worlds.   Possible Causes Scholars are divided concerning what caused the dust veil: a violent volcanic eruption—or several (see Churakova et al.), a cometary impact, even a near miss by a large comet could have created a dust cloud made up of dust particles, smoke from fires and (if a volcanic eruption) sulfuric acid droplets such as that described. Such a cloud would reflect and/or absorb light, increasing the earths albedo and measurably decreasing the temperature. Sources Arrhenius B. 2012. Helgà ¶ in the shadow of the dust veil 536-37. Journal of Archaeology and Ancient History 2013(5).Arjava A. 2005. The Mystery Cloud of 536 CE in the Mediterranean Sources. Dumbarton Oaks Papers 59:73-94.Baillie M. 2007. The case for significant numbers of extraterrestrial impacts through the late Holocene. Journal of Quaternary Science 22(2):101-109. doi: 10.1002/jqs.1099Baillie MGL, and McAneney J. 2015. Tree ring. Climate 11(1):105-114. effects and ice core acidities clarify the volcanic record of the first millennium of the PastChurakova OV, Bryukhanova MV, Saurer M, Boettger T, Naurzbaev MM, Myglan VS, Vaganov EA, Hughes MK, and Siegwolf RTW. 2014. A cluster of stratospheric volcanic eruptions in the AD 530s recorded in Siberian tree rings. Global and Planetary Change 122:140-150.Engvild KC. 2003. A review of the risks of sudden global cooling and its effects on agriculture. Agricultural and Forest Meteorology 115(3–4):127-137. doi:10.1016/s0168-1923(02 )00253-8Grà ¤slund B, and Price N. 2012. Twilight of the gods? The ‘dust veil event’ of AD 536 in critical perspective. Antiquity 332:428-443.Larsen LB, Vinther BM, Briffa KR, Melvin TM, Clausen HB, Jones PD, Siggaard-Andersen M, Hammer CU, Eronen M, and Grudd H. 2008. New ice core evidence for a volcanic cause of the AD 536 dust veil. Geophysical Research Letters 35(4)Rigby E, Symonds M, and Ward-Thompson D. 2004. A comet impact in AD 536? Astronomy Geophysics 45(1):1.23-1.26