Yue Li , Yougui Song , Xinzhou Li , Xiaoxun Xie , Dimitris G. Kaskaoutis , Jovid Aminov , Sodiqjon Yatimov
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引用次数: 0
Abstract
Dust activity in Central Asia (CA) holds significant scientific interest due to their broad social and environmental impacts. Loess deposits in CA serve as crucial natural archives, recording regional atmospheric characteristics and dust dynamics. The oldest loess in CA has been discovered in southern Tajikistan. However, debates persist regarding the wind dynamics of the Tajikistan loess deposition, which motivates our current study. By analyzing grain sizes of the last glacial loess and previous loess records since 800 ka, we determined that the Tajikistan loess consisted of post-storm floating dust and fine-grained dust transported by the westerlies. The reduced grain sizes may indicate less frequent dust storms. Our results provided explanation for the influence of global ice volume changes on the dust dynamics in southern Tajikistan, primarily by modulating sea-level pressure differences between the Caspian Sea and Hindu Kush/Pamirs. These ice volume changes also intensified rapid atmospheric fluctuations in CA, suggesting a sensitive response of the latter to glacial boundary conditions. Moreover, although precipitation variations may influence dust activities, their impact appears to be minimal. Collectively, our findings offer vital insights into the formation of loess strata and the development of extensive modern loess landforms in southern CA.
中亚(CA)的沙尘活动具有广泛的社会和环境影响,因此在科学上具有重要意义。中亚地区的黄土沉积是重要的天然档案,记录着区域大气特征和沙尘动态。中亚最古老的黄土是在塔吉克斯坦南部发现的。然而,关于塔吉克斯坦黄土沉积的风力动态一直存在争议,这也是我们当前研究的动机。通过分析末次冰川期黄土的粒度和 800 ka 年以来的黄土记录,我们确定塔吉克斯坦黄土由风暴后的浮尘和西风带来的细粒尘埃组成。颗粒尺寸的减小可能表明沙尘暴的频率降低了。我们的研究结果解释了全球冰量变化对塔吉克斯坦南部沙尘动力学的影响,主要是通过调节里海和兴都库什/帕米尔之间的海平面压力差。这些冰量变化也加剧了中亚地区大气的快速波动,表明后者对冰川边界条件的敏感反应。此外,尽管降水变化可能会影响沙尘活动,但其影响似乎微乎其微。总之,我们的研究结果为了解黄土地层的形成和加利福尼亚南部广泛的现代黄土地貌的发展提供了重要的启示。
期刊介绍:
Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.