评估土地利用变化对默斯河流域洪水的影响

A. De Roo, M. Odijk, G. Schmuck, E. Koster, A. Lucieer
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引用次数: 147

摘要

最近,世界几个地区发生了严重的洪水。为了研究洪水的成因以及土地利用、土壤特征和流域前期湿度条件的影响,开发了分布式流域模型LISFLOOD。LISFLOOD模拟大流域的径流。两个跨国欧洲河流流域被用来测试和验证该模型:默兹流域(法国、比利时、德国和荷兰)和奥德流域(捷克共和国、波兰和德国)。在默兹和奥德流域,目前正在处理过去200年的土地利用变化信息。LISFLOOD模拟模型用于模拟这些土地利用变化对洪水的影响。一些土地利用和植被对水分平衡的影响是明确的,如植被覆盖(叶面积指数)的变化会影响蒸散发。然而,植被对土壤特性的影响尚不清楚,土壤特性影响着入渗、土壤水分再分配、通流和地下水补给。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessing the effects of land use changes on floods in the meuse and oder catchment

Recently, dramatic flooding occurred in several regions of the world. To investigate the causes of the flooding and the influence of land use, soil characteristics and antecedent catchment moisture conditions, the distributed catchment model LISFLOOD has been developed. LISFLOOD simulates runoff in large river basins. Two transnational European river basins are used to test and validate the model: the Meuse catchment (France, Belgium, Germany and The Netherlands) and the Oder basin (The Czech Republic, Poland and Germany). In the Meuse and Oder catchment, land use change information over the past 200 years is processed at the moment. The LISFLOOD simulation model is used to simulate the effects of these land use changes on floods. Some influences of land use and vegetation on the water balance are clear, such as the changing vegetation cover (leaf area index) which will influence evapotranspiration. However, not so much is known about the influences of vegetation on soil properties, which influencesinfiltration, soil water redistribution, throughflow and groundwater recharge.

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