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首页> 外文期刊>Quaternary International >Riverbank migration and island dynamics of the braided Jamuna River of the Ganges—Brahmaputra basin using multi-temporal Landsat images
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Riverbank migration and island dynamics of the braided Jamuna River of the Ganges—Brahmaputra basin using multi-temporal Landsat images

机译:使用多时相Landsat影像的恒河—布拉马普特拉盆地辫状的Jamuna河的河岸迁移和岛屿动力学

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摘要

As one of the largest braided rivers in the world, the Jamuna River (JM) of the lower Brahmaputra regularly undergoes significant erosion, causing major bankline migration, making thousands of families homeless and sizeable land loss every year, e.g., the dynamic nature of Jamuna causes great suffering to the people living along its course and on its islands. Therefore, gaining a better understanding of the river's behavior should contribute to mitigate these sufferings and also to reduce the possible damage of the river to public infrastructure. In this study, using thirteen selected images of Landsat MSS and TM acquired from 1973 to 2003, the riverbank migration patterns and island dynamics of JM resulted from accretion/erosion processes for 30 years were investigated. For short-term analysis, the migration rate from one Landsat image to the next is estimated. For long-term analysis, the migration rates are based on the difference between the 1973 image as the reference, and subsequent images. For the short-term (long-term) analysis, the average erosion and accretion rates are 227 and 271 m/y (90 and 104 m/y) on the left bank, and 187 and 148 m/y (75 and 50 m/y) on the right bank of Jamuna, respectively. Because of human interventions and the averaging effect of erosion and accretion, the long-term migration rate is lower than that of the short-term migration rate on both banks. The short-term rate of accretion (erosion) on the left (right) bank follows the general pattern of river bank migration, while the accretion (erosion) of the right (left) bank does not follow such a pattern. On the other hand, the long-term erosion and accretion processes for both banks partly follow the general pattern of river bank migrations. From one flood to another, large islands tend to be more stable with little changes, but smaller islands underwent more changes. From results obtained from analyzing multi-temporal Landsat images, this study provides new and accurate information about the riverbank migration of JM.
机译:作为世界上最大的辫状河之一,下雅鲁藏布江的贾木纳河(JM)经常遭受严重侵蚀,导致大量银行迁徙,每年使成千上万的家庭无家可归,土地损失巨大,例如,贾木纳的动态性质给沿途及其岛屿生活的人民造成巨大的痛苦。因此,更好地了解河流的行为应有助于减轻这些痛苦并减少河流对公共基础设施的可能损害。在这项研究中,使用从1973年至2003年获得的13幅Landsat MSS和TM图像,调查了30年因增生/侵蚀过程引起的JM的河岸迁移模式和岛屿动态。对于短期分析,估计从一个Landsat图像到下一个Landsat图像的迁移率。对于长期分析,迁移率基于1973年作为参考的图像与后续图像之间的差异。对于短期(长期)分析,左岸的平均侵蚀和积聚速率分别为227和271 m / y(90和104 m / y),以及187和148 m / y(75和50 m / y) / y)分别位于Jamuna的右岸。由于人为干预以及侵蚀和增生的平均效应,两岸的长期迁移率均低于短期迁移率。左(右)河岸的短期增生(侵蚀)速率遵循河岸迁移的一般模式,而右(左)河岸的短期增生(侵蚀)速率不遵循这种模式。另一方面,两岸的长期侵蚀和增生过程部分遵循河岸迁徙的一般模式。从一次洪灾到另一次洪灾,大岛往往更稳定,几乎没有变化,但是较小的岛则经历了更多的变化。从分析多时相Landsat影像获得的结果来看,这项研究提供了有关JM河岸迁移的新的准确信息。

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  • 来源
    《Quaternary International》 |2012年第14期|p.148-161|共14页
  • 作者单位

    Civil and Environmental Engineering, University of Alberta, NREF 3-033, Edmonton, Alberta, Canada T6C 2W2;

    Civil and Environmental Engineering, University of Alberta, NREF 3-033, Edmonton, Alberta, Canada T6C 2W2;

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