确定大坝下游海岸线后退的多标准方法:北非案例

Q3 Earth and Planetary Sciences
O. Amrouni, G. Mahé
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引用次数: 1

摘要

摘要北非海滩是极端气候变化危害下最脆弱的地区之一。海岸主要是沉积的低洼平台,由陆地产量供应,但越来越多地被水坝打断。不幸的是,沉积物通量很少被测量和监测,因此今天几乎不可能评估大陆沉积物对海岸的贡献及其变化。我们研究的目的是确定三角洲沉积平原和近岸海底的采样方案,以便更好地了解与气候变化相比的人为驱动因素。我们采用了基于地貌特征和从河流到沿岸平原的历史演变的多准则分析。在人为变化后,海岸线的演变显示出惊人的后退趋势,达到- 20 m±0.15 m /年,其中约50%的泥沙流量被截流在大坝上游,包括几乎所有的粗质物质,如沙子。岸线的退缩和河流泥沙速率的降低都是由于大坝建设造成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multi-criteria approaches to identify the shoreline retreat downstream of dams: the North African case
Abstract. Northern African beaches are among the most vulnerable areas under the extreme climate change hazard. Mainly sedimentary low-lying platform, the coasts are supplied by terrestrial yields, which are increasingly interrupted by dams. Unfortunately, the sediment fluxes are rarely measured and monitored, so that it is quite impossible today to assess the contribution of continental sediments to the coast and its variability. The aim of our study is to determine the sampling protocol of delta sedimentation plain and nearshore seabed for better understanding of the anthropogenic driver in contrast to climate change. We adopt a multi-criteria analysis based both on the geomorphologic feature and the historic evolution from the River to the littoral plain. The shoreline evolution reveals an alarming retreat trend reaching −20 m ± 0.15 m yr−1 after the human-induced change where ∼50 % of sediment discharge has been trapped upstream the dam, including quite all the coarse material, like sand. The shoreline retreat and the decreasing sediment rate of fluvial flow are all due to the dam construction.
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来源期刊
Proceedings of the International Association of Hydrological Sciences
Proceedings of the International Association of Hydrological Sciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
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