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Suppression of precipitation by dust particles originated in the Tibetan Plateau,
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  • 相关项目：西昆仑山黄土与我国西北内陆的干旱化过程
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西昆仑山黄土与我国西北内陆的干旱化过程
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极端干旱区黄土土壤容重的测量及其古气候意义
西昆仑山黄土的岩石磁学特征及其磁化率增强机制
西宁盆地谢家剖面车头沟组底部木化石的发现及其意义
中国西北主要粉尘源区地表物质的常量元素分析
Dust aerosols: A possible accelerant for an increasingly arid climate in North China
Correlation between the magnetic susceptibility record of the Chinese aeolian sequences and the mari
Link between benthic oxygen isotopes and magnetic susceptibility in the red-clay sequence on the Chi
上新世- 第四纪亚洲内陆干旱化过程—柴达木中部鸭湖剖面孢粉和盐类化学指标证据
Shifts of dust source regions over central Asia and the Tibetan Plateau: Connections with the Arctic
Tibetan uplift intensified the 400 kyr signal in paleoclimate records at 4 Ma
surface-water freshening: A cause for the onset of North Pacific stratification from 2.75 Ma onward
青藏高原东部边缘“成都黏土”粒度记录的约500kaBP的干旱化增强事件