中文摘要：

基于记录在北方中央的中国从黄土存款导出的气候， paleomonsoonal 在迟了的更新世期间改变的东亚的特征如下被总结：(i)0.1 妈气候时期在东亚上在夏天和冬季 monsoonal 变化是占优势的；(ii ) 东亚 monsoonal 变化在迟了的更新世期间与印度季风不同；(iii ) 有一锝 ?-ka 时间相对理论上计算的太阳的放射变化东亚季风变化落后；(IV ) 向最后冻结成冰的夏天季风的冬季季风和减少的增加有一个一般趋势；在东亚 monsoonal 区域的(V) ， glacial-to-interglacial 周期的振幅从南方显示出显著增加到北方。解释这些特征，一个概念的模型被开发， monsoonal 历史上强迫全球冰体积变化被强调。

英文摘要：

Based on the climate records derived from loess deposits in north-central China, the characteristics of the East-Asia paleomonsoonal changes during the Late Pleistocene are summarized as follows: (i) The 0.1-Ma climate period is predominant in both summer and winter monsoonal changes over East Asia; (ii) The East-Asia monsoonal variation is different from the Indian monsoon during the Late Pleistocene; (iii) There is a ～5-ka time lag of the East-Asia monsoon changes relative to the theoretically calculated solar radiation changes; (IV) There is a general trend toward increase in winter monsoon and decrease in summer monsoon in the last glaciation; (V) In the East-Asia monsoonal region, the amplitude of glacial-to-interglacial cycles shows a remarkable increase from south to north. To explain these characteristics, a conceptual model is developed and the forcing of global ice volume variations in the monsoonal history is emphasized.