Extreme erosion in the Changjiang subaqueous delta caused by intensification of storms during the Medieval Warm Period
编号:1599 访问权限:仅限参会人 更新:2024-10-15 15:02:24 浏览:209次 口头报告

报告开始:2025年01月15日 16:35(Asia/Shanghai)

报告时间:15min

所在会场:[S53] Session 53-Geological Analogues for Future Warm Ocean and Cimate [S53-1] Geological Analogues for Future Warm Ocean and Climate

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摘要
River deltas play a crucial role in coastal zones. However, with the increase in human activities, accelerated sea level rise, and extreme weather events, the world's major river deltas are increasingly threatened by erosion and degradation. As one of the most densely populated areas in China, the Changjiang Delta has undergone erosion and siltation transformation in recent decades, with an increased risk of erosion. Among them, the erosion of subaqueous deltas has received a lot of attention. The existing studies mostly focus on the erosion of modern (tidal to decadal scale) process, but there is a lack of systematic understanding of erosion processes over longer time scales, especially in the deltaic progradation evolution cycle. Furthermore, the stratigraphic expression of erosion processes at various time scales is still unclear. In this study, a large number of high-resolution sub-bottom profiles and core data, combined with historical records, are used to attempt to discuss and quantify the response of the Changjiang subaqueous delta to paleo-storm events. Our analysis reveals that the Changjiang subaqueous delta has an obvious depositional discontinuity at ~0.8-1.4 ka BP, which occurs at burial depths ranging from ~20 m to ~30 m while extending deeper toward offshore areas until it pinches out around 30 m depth. At the same time, the accumulation of shell layers in several cores during this period indicates a storm-led erosion process, which may reach ~ 5500 km2. While many paleoclimatic records show that the frequency of stroms in the eastern shelf of China and its adjacent areas increased significantly during the Medieval Warm Period, which provided strong hydrodynamic conditions for the occurrence of erosion. At the same time, the Changjiang basin has experienced aridity, which has also led to a reduction in sediment recharge in the estuarine area, thereby intensifying erosion. In light of current global warming and the doubling of storm intensity indices over nearly 40 years, river deltas that are already deficient in sediment recharge will confront increasingly severe erosion challenges. This study provides valuable insights into the erosion processes affecting the delta within the context of climate change, and it is crucial not to overlook the potential impacts of extreme weather on these deltas in the future.
 
关键词
Changjiang subaqueous delta,erosion,subbottom profile,paleo-strom
报告人
Wei Feng
Postdoctor Nanjing Normal University

稿件作者
Wei Feng Nanjing Normal University
Shihao Liu East China Normal University
Ya Ping Wang Nanjing University;East China Normal University
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重要日期
  • 会议日期

    01月13日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 01月17日 2025

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
承办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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