目的在确定末次盛冰期时古黑潮流域模式以及海陆气候相互作用。
Our objective is to examine the shift in the path of the Kuroshio and the interaction be-tween land and sea during the last glacial maximum (LGM).
但相对于末次盛冰期气候的变化，这两个因子的贡献都是比较小的。
However, both factors have rather small contributions to the climate change in the LGM.
末次盛冰期以来南海南部海平面及海洋底水温度均发生了很大的变化。
There has been a big change of the sea level and seabed water temperature since the Last Glacial Maximum (LGM) in southern south China sea.
它使得中国东部地区降水减少，由此造成的降水减少占末次盛冰期降水减少的25%—50%。
The impact on precipitation in the east coastal region of China was most significant, accounting for 25%-50% of the total precipitation reduction during the LGM.
它使得中国东部地区降水减少，由此造成的降水减少占末次盛冰期降水减少的25%—50%。
The impact on precipitation in the east coastal region of China was most significant, accounting for 25%-50% of the total precipitation reduction during the LGM.
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