In the Late Tertiary and Quaternary the climate systems of China and Australia have become increasingly linked due to the monsoon and trade wind circulation patterns across the equatorial region.
穿越赤道区的季风和信风的环流格局,致使新第三纪和第四纪中国与澳大利亚的气候系统的相关性更强。
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Since the beginning of the Quaternary, with the uplift of Tibetan Plateau, the Asian monsoon was established and became the controlling factor of the climate and environmental change of China.