文献类型：期刊文献

英文题名：Impacts of El Nino-Southern oscillation on multi-scale morphodynamics of an embayed beach in southern China

作者：Hu, Taihuan[1];Zhu, Shibing[2,3];Chen, Shenliang[1];Chen, Zhaoguang[2];Li, Zhiqiang[2]

机构：[1]East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai, Peoples R China;[2]Guangdong Ocean Univ, Coll Elect & Informat Engn, Zhanjiang, Peoples R China;[3]Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing, Peoples R China

年份：2025

卷号：137

外文期刊名：PHYSICS AND CHEMISTRY OF THE EARTH

收录：SCI-EXPANDED(收录号：WOS:001361155000001)、、WOS

基金：Funding This work was funded by the National Natural Science Foundation of China (Grant No. 4217616, 41,676,079) and the Science and Technol-ogy Basic Investigation Program of China (Grant No. 2022FY202404) .

语种：英文

外文关键词：Embayed beach; Shoreline change; Morphodynamics; ENSO; Storm event

外文摘要：Increased coastal erosion and extreme oceanographic forcing driven by El Nino-Southern Oscillation (ENSO) along the Pacific coast are increasingly receiving concerns. Despite considerable attention, the specific impact of these phenomena on Chinese shorelines, particularly along the South China beaches, remains inadequately understood. To address this gap, this study conducted high-frequency surveys on the Qing'an Bay beach in South China and employ a profile fitting model to refined waterline extraction from monthly satellite images. The goal was to investigate the relationship between high-frequency shoreline changes and interannual climate variability (such as ENSO). The findings indicate that the coastal evolution is intricately linked to a combination of strong wave events, summer storms, winter cold waves, and the amplifying effects of ENSO. During La Nina phase, the sea level in the western Pacific experiences a rise, with associated storms proving particularly destructive to the beach environment, leading to violent oscillations in the coastline. Specifically, in the strong La Nina phases, significant wave heights markedly surpass neutral conditions, precipitating intensified sediment movement. However, it is imperative to recognize that shoreline changes alone do not fully characterize coastal erosion. Assessment must also encompass alterations in beach volume. By calculating beach volume per unit width that accounts for the influence of ENSO variability on the beach, the seasonal characteristics of the beach showed sediment losses in summer and autumn, and gains in winter and spring, which was more obvious during strong La Nina. Additionally, conceptual model analysis reveals that during the La Nina phase, the bay is fully exposed, whereas during the El Nino phase, significant headland sheltering is observed.