The Azimuth Project
Allerød (changes)

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Idea

The Allerød period or Allerød oscillation was a warm and moist global interstadial? beginning around 12,000-11,000 BC, after the end of the last glacial period?. The Allerød raised temperatures in the northern Atlantic region to almost present-day levels before they declined again in the Younger Dryas.

In some regions, especially northern Eurasia, there is evidence for a cold period known as the Older Dryas? interrupting this interstadial. In such regions the shorter warm period ending with the Older Dryas is called the Bølling, and the term ‘Allerød’ is reserved for the warm period after the Older Dryas.

References

category: climate

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