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首页> 外文期刊>Journal of Hydrology >Sustained growth of river-mouth bars in the vulnerable Changjiang Delta
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Sustained growth of river-mouth bars in the vulnerable Changjiang Delta

机译:脆弱的长江三角洲河口坝持续增长

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Based on 345 satellite images from 1991 to 2018, we examine the height, area and morphological changes of two large newborn river-mouth bars in the vulnerable Changjiang Delta as well as their influencing factors. The growth of inaccessible river-mouth bars is less affected by human estuarine activities, therefore, studying their growth shows particular promise in revealing the effects of relative sea level rise and human activities upstream of the river basin. We find the morphologic changes of the river-mouth bars in the Changjiang Delta are seriously affected by waves, tides and runoff, but their height and area growth depends on whether there is sufficient river sediment supply, and the impact of relative sea level rise is relatively small. The river-mouth bar located in the active distributary mouth has maintained rapid growth in the past three decades, although the Three Gorges Dam has trapped most of the upstream sediment. We believe it is the sediment scoured from the main channel downstream of the dam substantially supplements the sediment discharged to the sea, contributing to the rapid growth of the river-mouth bar. Our finding inspires a reassessment of the effects of dam construction on delta evolution when sediment reserves downstream of the dam are large and the runoff is ample. Under the current circumstances of rapid sea level rise and intensified human activities, the rapid growth of river-mouth bars mainly due to the sediment supply from the river channels allows precious buffer time to protect the vulnerable Changjiang Delta, and it also brings hope for and new perspectives on the protection of other major deltas in the world.
机译:本文以1991—2018年的345颗卫星遥象为基础,研究了脆弱的长江三角洲两条新生大型河口坝的高度、面积和形态变化及其影响因素。难以进入的河口坝的生长受人类河动的影响较小,因此,研究它们的生长在揭示相对海平面上升和河流流域上游人类活动的影响方面显示出特别的前景。研究发现,长江三角洲河口坝的形态变化受波浪、潮汐和径流影响较严重,但其高度和面积增长取决于河流泥沙供应是否充足,相对海平面上升的影响相对较小。位于活跃支流口的河口坝在过去三十年中保持了快速增长,尽管三峡大坝捕获了大部分上游沉积物。我们认为,正是从大坝下游主河道冲刷的沉积物大大补充了排入大海的沉积物,促成了河口坝的快速增长。我们的发现激发了对大坝建设对三角洲演化影响的重新评估,当大坝下游的沉积物储量很大且径流充足时。在当前海平面快速上升和人类活动加剧的情况下,主要由于河道的泥沙供应,河口坝的快速增长为保护脆弱的长江三角洲提供了宝贵的缓冲时间,也为保护世界其他主要三角洲带来了希望和新视角。

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