Through comprehensive analysis of the climate in the latePleistocene Epoch was found to be cold and humid during the glacial stagesand warm and dry in the interglacial stages.
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释义
即表现为冰期冷湿与间冰期暖干的气候型。从此取代了早、中更新世的与东部季风区相似的冷干与暖湿相结合的气候型。
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