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Climate or Land Use?—Attribution of Changes in River Flooding in the Sahel Zone

机译:气候还是土地利用?-萨赫勒地区河流洪水变化的归因

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This study intends to contribute to the ongoing discussion on whether land use and land cover changes (LULC) or climate trends have the major influence on the observed increase of flood magnitudes in the Sahel. A simulation-based approach is used for attributing the observed trends to the postulated drivers. For this purpose, the ecohydrological model SWIM (Soil and Water Integrated Model) with a new, dynamic LULC module was set up for the Sahelian part of the Niger River until Niamey, including the main tributaries Sirba and Goroul. The model was driven with observed, reanalyzed climate and LULC data for the years 1950–2009. In order to quantify the shares of influence, one simulation was carried out with constant land cover as of 1950, and one including LULC. As quantitative measure, the gradients of the simulated trends were compared to the observed trend. The modeling studies showed that for the Sirba River only the simulation which included LULC was able to reproduce the observed trend. The simulation without LULC showed a positive trend for flood magnitudes, but underestimated the trend significantly. For the Goroul River and the local flood of the Niger River at Niamey, the simulations were only partly able to reproduce the observed trend. In conclusion, the new LULC module enabled some first quantitative insights into the relative influence of LULC and climatic changes. For the Sirba catchment, the results imply that LULC and climatic changes contribute in roughly equal shares to the observed increase in flooding. For the other parts of the subcatchment, the results are less clear but show, that climatic changes and LULC are drivers for the flood increase; however their shares cannot be quantified. Based on these modeling results, we argue for a two-pillar adaptation strategy to reduce current and future flood risk: Flood mitigation for reducing LULC-induced flood increase, and flood adaptation for a general reduction of flood vulnerability.
机译:这项研究旨在促进有关土地利用和土地覆盖变化(LULC)或气候趋势是否对观测到的萨赫勒地区洪水强度增加有重大影响的持续讨论。基于模拟的方法用于将观察到的趋势归因于假定的驱动因素。为此,在尼日尔直到萨摩亚(包括主要支流Sirba和Goroul)建立了带有新的动态LULC模块的生态水文模型SWIM(土壤和水的综合模型)。该模型是由观测,重新分析的气候和1950-2009年的LULC数据驱动的。为了量化影响的份额,从1950年开始,在恒定土地覆盖率下进行了一次模拟,其中一次包括LULC。作为定量度量,将模拟趋势的梯度与观察到的趋势进行比较。建模研究表明,对于锡尔巴河,只有包括LULC在内的模拟才能重现观测到的趋势。没有LULC的模拟显示洪水幅度呈正趋势,但明显低估了趋势。对于Goroul河和Niamey尼日尔河的局部洪水,模拟仅能部分再现观测到的趋势。总之,新的LULC模块使人们对LULC和气候变化的相对影响有了一些初步的定量见解。对于Sirba流域,结果表明LULC和气候变化在洪水泛滥方面所占份额大致相等。对于子汇水面积的其他部分,结果虽然不太清楚,但显示出气候变化和土地利用变化和土地变化是洪水泛滥的驱动因素。但是他们的份额无法量化。基于这些建模结果,我们提出了一种减少当前和未来洪水风险的两支柱适应策略:减轻洪水以减少LULC引起的洪水增加,以及通过洪水适应来总体减少洪水的脆弱性。

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