Morphological changes in the offshore islands of Meghna estuary: Analysis of the erosion and accretion dynamics

Fariha Khatun, Ovi Ranjan Saha, Naila Matin
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引用次数: 0

Abstract

This study examines the morphological changes of ten offshore islands in the Meghna estuary of Bangladesh over thirty years, from 1989 to 2019, utilizing remote sensing and Geographic Information System (GIS) techniques. The study area, characterized by ever-changing hydrodynamic conditions due to the substantial discharge from the Ganges, Jamuna, and Meghna rivers, experiences significant sediment deposition and erosion. Our findings highlight a complex interplay between erosion and accretion processes across the estuary. Despite 1100 km2 of land being eroded, accretion processes were slightly more predominant, totaling 1210 km2, resulting in a net increase of 110 km2 in land area. Notably, islands like Swarna Dwip and Moulovi Char exhibited substantial land gains, while Manpura and the eastern part of Bhola experienced significant reductions, underlining the urgent need for targeted erosion mitigation strategies. The study also identifies significant sediment deposition near tidal confluence zones around Sandwip, Jahazer Char, and Urir Char, suggesting that these are key areas for conservation efforts. The research contributes valuable insights into the geomorphological dynamics within the Meghna estuary. It offers foundational knowledge for informed coastal management and sustainable development planning in one of the world's most dynamically evolving coastal environments.
梅克纳河口近海岛屿的形态变化:侵蚀和吸积动力学分析
利用遥感和地理信息系统(GIS)技术,研究了1989年至2019年孟加拉国梅克纳河河口10个近海岛屿30年来的形态变化。由于恒河、贾穆纳河和梅克纳河的大量流量,研究区域的水动力条件不断变化,经历了大量的泥沙沉积和侵蚀。我们的发现强调了河口侵蚀和增生过程之间复杂的相互作用。尽管有1100 km2的土地被侵蚀,但增积过程略占优势,总计1210 km2,导致土地面积净增加110 km2。值得注意的是,斯瓦纳德威普岛和莫洛维查尔岛等岛屿的土地面积大幅增加,而曼普拉岛和博拉岛东部的土地面积则大幅减少,这突出表明迫切需要制定有针对性的减缓侵蚀战略。该研究还发现,在Sandwip、Jahazer Char和Urir Char附近的潮汐汇流带附近有大量沉积物沉积,这表明这些是保护工作的关键区域。该研究为研究梅克纳河河口的地貌动态提供了有价值的见解。它为世界上最动态发展的沿海环境之一的知情沿海管理和可持续发展规划提供了基础知识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
9.20
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