US-China Collaborative Study of Holocene Paleoclimatology

黄土序列提供了大气中气溶胶浓度和陆地干旱历史的极好记录。最适合研究的黄土层序是中国，那里在全新世沉积了多达10米的沉积物。在整个时间间隔内，14C测年技术提供了准确的沉积历史年表；因此，可以准确地确定陆地气候变化与气候系统的其他组成部分(冰量、海洋表面和深水温度)之间的时间关系。这项建议将研究中国在一个对亚洲季风反应敏感的地区的气候历史。这很重要，因为它将有助于我们更好地了解全新世早期季风环流加强的区域影响和年代学，北印度洋沉积物岩芯和附近的热带高山冰芯已经记录了这一点。

Loess sequences provide excellent records of aerosol concentrations in the atmosphere and the history of terrestrial aridity. The best loess sequences for study are in China, where as much as 10 meters of sediments were deposited in the Holocene. Throughout this interval of time, 14C dating techniques provide accurate chronologies of the sedimentation history; thus the temporal relationship between terrestrial climate change and other components of the climate system (ice volume, marine surface and deep water temperatures) can be accurately determined. This proposal will study the history of climate in China in a region with a sensitive response to the Asian monsoon. It is important because it will help to improve our understanding of the regional impact and chronology of the early Holocene intensification of monsoonal circulation, already documented in northern Indian Ocean sediment cores and nearby, tropical alpine ice cores.