Dwivedi Deepika, Mani Murali R, Mishra Puneet Kumar
CSIR-National Institute of Oceanography, Dona Paula, Goa, 403004, India; Academy of Scientific and Innovative Research (AcSIR), Ghaziabad, 201002, India.
CSIR-National Institute of Oceanography, Dona Paula, Goa, 403004, India; Academy of Scientific and Innovative Research (AcSIR), Ghaziabad, 201002, India.
Mar Pollut Bull. 2026 Jan;222(Pt 1):118653. doi: 10.1016/j.marpolbul.2025.118653. Epub 2025 Sep 8.
The Indian Sundarban Delta (ISD), located at the confluence of the Ganga-Brahmaputra-Meghna river system along India's eastern coast, is among the world's most geomorphologically dynamic and environmentally vulnerable deltaic systems. Over the past five decades, the region has undergone substantial morphodynamic changes driven by natural forces such as relative sea-level rise, wave action, and sediment flux, as well as anthropogenic factors like upstream water regulation via dams and barrages. This study examines the long-term evolution of shoreline and island morphology across the ISD from 1972 to 2025 using multi-temporal Landsat datasets under consistent tidal conditions. Shorelines were manually digitized and analyzed using the Digital Shoreline Analysis System (DSAS) in ArcGIS. A total of 45,356 transects were generated at 50 m intervals across eight coastal zones, covering approximately 2980 km of shoreline. Shoreline dynamics were assessed using Net Shoreline Movement (NSM) and End Point Rate (EPR), which ranged from -3286 m to +4510 m and -62.97 m/year to +125.75 m/year, respectively. Additionally, Areal analysis of 92 tidal islands revealed a net land loss of 72 km, driven by 256.31 km of erosion and partly balanced by 183.88 km of accretion. Ocean-facing island margins displayed the highest morphodynamic instability and erosion rates. Notably, the emergence of several new sand patches suggests localized deposition that could develop into stable landforms under favorable conditions. These spatial-temporal trends are closely linked to sea-level rise, upstream sediment retention, swell wave dominance, and increased cyclone frequency, underscoring the need for integrated coastal management.
印度孙德尔本斯三角洲(ISD)位于印度东海岸恒河-布拉马普特拉河-梅克纳河水系的交汇处,是世界上地貌最活跃、环境最脆弱的三角洲系统之一。在过去的五十年里,该地区经历了巨大的地貌动力变化,这些变化是由相对海平面上升、海浪作用和泥沙通量等自然力以及诸如通过大坝和水坝进行上游水调节等人为因素驱动的。本研究利用多期陆地卫星数据集,在一致的潮汐条件下,研究了1972年至2025年期间ISD海岸线和岛屿形态的长期演变。使用ArcGIS中的数字海岸线分析系统(DSAS)对手动数字化的海岸线进行了分析。在八个沿海区域以50米的间隔共生成了45356条横断面,覆盖了约2980公里的海岸线。使用净海岸线移动(NSM)和终点速率(EPR)评估海岸线动态,其范围分别为-3286米至+4510米和-62.97米/年至+125.75米/年。此外,对92个潮汐岛的面积分析显示,净陆地损失72公里,其中侵蚀256.31公里,部分由183.88公里的淤积平衡。面向海洋的岛屿边缘表现出最高的地貌动力不稳定性和侵蚀速率。值得注意的是,几个新沙洲的出现表明存在局部沉积,在有利条件下可能发展成稳定的地貌。这些时空趋势与海平面上升、上游泥沙滞留、涌浪主导和飓风频率增加密切相关,突出了综合海岸管理的必要性。