Allerød oscillation
（重定向自Allerod Oscillation）
The Allerød oscillation (Danish:Allerødtiden) was a warm and moist global interstadial that occurred at the end of the last glacial period. It raised temperatures in the northern Atlantic region to almost present-day levels, before they declined again in the succeeding Younger Dryas period, which was followed by the present interglacial period.