Hydrological and morphological responses in the São Francisco River Basin (Northeast Brazil) resulting from river damming and climate changes in a tropical region

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Pedro Victor Oliveira Gomes, Felipe Torres Figueiredo, Gelson Luís Fambrini, Fabiano Pupim, Carlos Henrique Grohmann, Luiz Alberto Vedana, Luisa Sampaio Franco
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Abstract

The São Francisco River in Northeast Brazil has seen hydrological and morphological changes due to extensive damming and climate change over the past century. In this study, we examine the influence of human activities and natural fluctuations in precipitation on the hydrological patterns of the basin and the morphological responses of the lower course of the river (LOW-SF) to these alterations over a span of several decades. The findings indicate a decrease in water release by 41% from 1995 to 2013 and 54% from 2013 to 2018, solely attributed to human actions. Furthermore, the operation of the reservoirs of the large dams resulted in a reduction in hydrological seasonality. The changing hydrological regime caused morphological changes that resulted in an expansion of the exposed subaerial fluvial bars in the LOW-SF and a reduction in channel width. As a result, the abandonment of small secondary channels occurred, leading to the cessation of inundation in previously buried elevated portions of bars, even during certain seasons. Another important factor was the spread of morphological changes in the LOW-SF, which started from the areas farthest from the last dam in the series of large dams, the Xingó Dam, and spread to the nearby regions. This is due to the lack of major tributaries in the semiarid region of the LOW-SF. The integrated assessment presented in this study illustrates both natural and anthropogenic influences. Moreover, in light of projected declines in precipitation, it is anticipated that natural phenomena could result in a substantial 73% decrease in water flow by the mid-20th century. This climatic scenario will lead to increased utilization of hydroelectric plants and more stringent control of water flow downstream of the dam cascade, intensifying the already documented adverse effects and posing the possibility of novel morphological adaptations.

Abstract Image

热带地区筑坝和气候变化对奥弗朗西斯科河流域(巴西东北部)水文和形态的影响
在过去的一个世纪里,由于大规模的筑坝和气候变化,巴西东北部的奥弗朗西斯科河经历了水文和形态的变化。在这项研究中,我们研究了人类活动和自然降水波动对流域水文模式的影响,以及河流下游(LOW-SF)对这些变化的形态响应。研究结果表明,仅由于人类活动,1995年至2013年的放水量减少了41%,2013年至2018年的放水量减少了54%。此外,大型水坝水库的运行导致水文季节性的减少。水文环境的变化引起了地形的变化,导致低顺水带暴露的陆上河坝扩大,河道宽度减小。结果,小的次级河道被遗弃,导致以前被埋的沙洲高架部分停止被淹没,甚至在某些季节也是如此。另一个重要的影响因素是低sf区形态变化的扩散,这种变化从离最后一座大坝Xingó大坝最远的地方开始,向附近地区扩散。这是由于在LOW-SF的半干旱地区缺乏主要的支流。本研究提出的综合评估说明了自然和人为影响。此外,鉴于预估的降水减少,预计到20世纪中叶,自然现象可能导致水流量大幅减少73%。这种气候情景将导致水力发电厂的利用率增加,对大坝下游水流的控制更加严格,加剧了已经记录的不利影响,并提出了新的形态适应的可能性。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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