Alternating dominance of Westerlies and East Asian winter monsoon on dust activities across the northeastern Qinghai-Tibet Plateau since 18.5 ka

IF 4 1区 地球科学 Q1 GEOGRAPHY, PHYSICAL Global and Planetary Change Pub Date : 2024-12-20 DOI:10.1016/j.gloplacha.2024.104684
Hao Long, Yun Cai, Jingran Zhang, Liangqing Cheng, Linhai Yang, Hongyi Cheng
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Abstract

The mid-latitude Westerlies and the East Asian winter monsoon (EAWM) are two major atmospheric circulation systems influencing dust activities in the Northern Hemisphere (NH). However, the interplay between these wind systems and their effects on regional dust activities remain poorly understood. In this study, we present a well-dated aeolian sedimentary sequence from the loess section (ZES) on the southern slope of the Qilian Mountains in the northeastern Qinghai-Tibetan Plateau (NE-QTP). It provides insights into the response of dust activities to these wind systems for the last 18.5 ka. We developed a detailed chronology for ZES section based on luminescence dating of multiple signals from 29 samples (yielding a total of 87 ages). The luminescence sensitivities and element analysis of the sediments indicate a shift in dust source around 7.5 ka, contributed to a transition in the atmospheric circulation controls of the NE-QTP. Specially, our findings suggest that dust activity was likely dominated by EAWM from 18.5 ka to 7.5 ka and by the Westerlies after 7.5 ka across this area. We propose that increased NH ice volume (NHIV) significantly enhanced the EAWM via strengthening Siberian High, driving dust activities over the high mountains during the Last Deglaciation and Early Holocene. In contrast, as NHIV decreased during the middle-to-late Holocene, the EAWM weakened and retreated from this area, allowing the Westerlies to dominate dust activities. Additionally, grain-size parameters of sediments were used to infer variations in the intensities of these winds, revealing a gradual weakening of EAWM since the Last Deglaciation and a marked intensification of the Westerlies during the warm middle Holocene. Under the current global warming scenario, we predict that the Westerlies will continue to dominate dust activities across the NE-QTP, with a potential increase in dust activities if the Westerlies enhance.
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18.5 ka以来西风带与东亚冬季风交替优势对青藏高原东北部沙尘活动的影响
中纬度西风带和东亚冬季风是影响北半球沙尘活动的两个主要大气环流系统。然而,这些风系统之间的相互作用及其对区域沙尘活动的影响仍然知之甚少。本文研究了青藏高原东北部祁连山南坡黄土剖面(ZES)的风成沉积层序。它提供了对过去18.5 ka的尘埃活动对这些风系统的响应的见解。基于29个样品的多个信号的发光测年(共产生87个年龄),我们开发了一个详细的ZES切片年表。沉积物的发光灵敏度和元素分析表明,在7.5 ka左右,沙尘源发生了转变,导致东北-青藏高原大气环流控制的转变。特别地,我们的研究结果表明,在18.5 ka至7.5 ka期间,该地区的沙尘活动可能以EAWM为主,7.5 ka之后则以西风带为主。最后一次消冰期和全新世早期,NHIV的增加通过增强西伯利亚高压,驱动高山沙尘活动而显著增强了EAWM。而在全新世中后期,随着NHIV的减少,EAWM减弱并从该地区撤退,使西风带主导了沙尘活动。此外,利用沉积物粒度参数来推断这些风的强度变化,揭示了末次消冰期以来EAWM逐渐减弱,而全新世中期温暖期西风带明显增强。在目前全球变暖的情况下,我们预测西风带将继续主导东北高原的沙尘活动,如果西风带增强,沙尘活动可能会增加。
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来源期刊
Global and Planetary Change
Global and Planetary Change 地学天文-地球科学综合
CiteScore
7.40
自引率
10.30%
发文量
226
审稿时长
63 days
期刊介绍: The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems. Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged. Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.
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