基于DSAS的江苏中部海岸线45年变化研究

IF 1.6 Q4 ENVIRONMENTAL SCIENCES Anthropocene Coasts Pub Date : 2023-03-20 DOI:10.1139/anc-2020-0001
Yuan Song, Yongming Shen, Ruofan Xie, Jialin Li
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引用次数: 3

摘要

苏中沿海地区分布着一个大型沙脊群,近岸地区发育有沉积淤泥质海堤。海岸线变化的定量监测对滩涂开发和保护具有重要意义。本研究提取了江苏中部沿海6个时期(1973–2018)的海岸线,并分析了其多年来的长度变化。数字海岸线分析系统(DSAS)用于生成垂直于基线的横截面,并计算海岸线的线性回归率(LRR)、终点率变化(EPR)和净海岸线移动(NSM),在此基础上分析海岸线变化特征。DSAS结果表明,研究区域的海岸线保持波动增长,并呈现出向海洋持续推进的趋势。从1973-2018年海岸线演化距离的变化来看,以2003-2013年为时间边界,研究区前进海岸线占总海岸线的50%以上,呈现先上升后下降的趋势。平均海岸线变化率为207米/年,变化程度最高的时期为1983-1993年和1993-2013年。2013-2018年,海岸线变化趋于稳定,只有少数河口和港口发生了明显的侵蚀和沉积。
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A DSAS-based study of central shoreline change in Jiangsu over 45 years

A large-scale sand ridge group is distributed in the central Jiangsu coastal area, and a deposition muddy sea bank was developed in the nearshore area. Quantitative monitoring of coastline changes is of great significance for tidal beach development and protection. The shorelines of the central coast of Jiangsu within six periods (1973–2018) were extracted in this study, and their length changes over the years were analyzed. The Digital Shoreline Analysis System (DSAS) was employed to generate a cross section perpendicular to the baseline and calculate the linear regression rate (LRR) of the shoreline, changes in end point rate (EPR), and net shoreline movement (NSM), based on which the shoreline change features were analyzed. The DSAS results indicated that the shorelines in the study area maintained fluctuating growth and presented a continuous advancing trend towards the sea. From the changes in shoreline evolution distance during 1973–2018, the advancing shorelines in the study area accounted for over 50% of the total shorelines and presented first rising and then declining trends with the period of 2003–2013 taken as the time boundary. The average shoreline change rate was 207 m/year, and the periods with the highest change degrees were 1983–1993 and 1993–2013. The shoreline change tended to be stable during 2013–2018, and only a few estuaries and ports underwent obvious erosion and sedimentation.

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