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内蒙古合同察汗淖碱湖的磁化率和稳定同位素资料的初步证据表明，在东北亚也经历了新仙女木（ＹｏｕｎｇｅｒＤｒｙａｓ）寒冷事件。此外，９０００～６０００ａＢＰ的潮湿气候环境可能是由于季风活动加剧所致，随后，一个逐渐干化的气候条件一直延续到现在。
Preliminary evidence of magnetic susceptibility and stable isotopic data from the Chahanu Lake in Inner Mongolia indicates that the cold weather in Younger Dryas has also been experienced in Northeast Asia. In addition, the humid climate of 9000-6000 aBP may be due to the intensification of monsoon activity, followed by a gradual drying of climatic conditions have continued until now.