基于地理空间技术和DSAS扩展的孟加拉国沿海岛屿岸线时空移动模拟

M. Salauddin, Khandaker Tanvir Hossain, Istiaqe Ahmed Tanim, Md. Anisul Kabir, Mehedi Hasan Saddam
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引用次数: 15

摘要

利用多时相卫星图像和GIS技术,对孟加拉国梅克纳河河口新形成岛屿的海岸线和侵蚀增积变化进行了研究。目前的研究使用NDWI和MNDWI来划定陆地和水域边界,提取海岸线,并使用一些覆盖分析来测量侵蚀-增积。利用DSAS扩展分析了岸线的移动。结果(1990-2015)表明,该岛在这段时间内增加了1192公顷的土地,在这段时间内,大约有1公里的海岸线因少数地方断裂而消失。大部分增生在西北部,侵蚀在东南部和西南部。将研究区划分为4个不同的区段,共构建了115个样带,其中向海运动样带74个,向陆运动样带44个。西北地区向海移动和岸线移动速率较大,净岸线移动(NSM)为+1897 m/年,终点速率(EPR)为+73 m/年。东南和西南向陆地移动和岸线移动速率较大,净岸线移动(NSM)约为-2680 m/年,终点速率(EPR)约为-129 m/年。最高向陆移动为-2680米,最高向海移动为+1897米。部分地区以冲积作用为主,侵蚀作用使岸线中断。
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Modeling Spatio-Temporal Shoreline Shifting of a Coastal Island in Bangladesh Using Geospatial Techniques and DSAS Extension
Abstract The study attempted to assess the changes in shoreline and erosion-accretion of newly formed island at the mouth of the Meghna river estuary in Bangladesh using multi temporal satellite images and GIS techniques. The current study used NDWI an MNDWI to delineate land and water boundary to extract the shoreline and also used some overlay analysis to measure the erosion-accretion. DSAS extension is used for analyzing the shifting of the shoreline. The results (1990-2015) show that the island has 1192 hectares of land accreted during this time period, and about 1 km of its shoreline lost during this time period as it has broken in few places. Most accretion found in the northwestern part and erosion in southeastern and southwestern part. The study area was divided into four different segments and about 115 transects were constructed, of which about 74 shows the seaward movement and 44 shows landward movement. Seaward movement and rate of shoreline shifting is higher in the northwestern part where net shoreline movement (NSM) is +1897 meters and end point rate (EPR) is +73 m/year. Landward movement and the rate of shoreline shifting are higher in southeastern and southwestern part of which net shoreline movement (NSM) is about -2680 meters and end point rate (EPR) is about -129 m/year. The highest landward movement is found as -2680 meters and highest seaward movement as +1897 meters. Accretion process is dominant while erosion process discontinued the shoreline in some places.
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