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Volcanic Winter of 536

Paleoclimatology

The volcanic winter of 536 was one of the most severe and prolonged episodes of climatic cooling in the Northern Hemisphere in the last two thousand years, triggered by at least one large volcanic eruption, of disputed origin, that injected sulfate aerosols into the atmosphere in late 535 or early 536. Contemporary observers in Constantinople described the sun losing its brightness and a persistent dry fog, and summer temperatures in 536 fell as much as 2.5 degrees Celsius below the European norm, with snow reported falling in August in China. The resulting crop failures and famine, compounding with the Plague of Justinian that struck beginning in 541, caused millions of deaths and ushered in the Late Antique Little Ice Age, a cold period that persisted from 536 to about 660.

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Caused By

Volcanism, Processes
Source Volcanic winter of 536 (Wikipedia)

In Discipline

Source Volcanic winter of 536 (Wikipedia)
Sources
Volcanic winter of 536 (Wikipedia)
  • In Discipline: Paleoclimatology, Lead paragraph (in-discipline)
    The volcanic winter of 536 was among the most severe and protracted episodes of climatic cooling in the Northern Hemisphere in the last two thousand years.
  • Caused By: Volcanism, Lead paragraph (caused-by)
    The volcanic winter was caused by at least three eruptions of uncertain origin, with several possible locations proposed in various continents.
  • In Group: Abrupt Climate Events, Lead sentence
    The volcanic winter of 536 was among the most severe and protracted episodes of climatic cooling in the Northern Hemisphere in the last two thousand years.
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