首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Modelling dynamic water redistribution patterns in arid catchments in the Negev Desert of Israel
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Modelling dynamic water redistribution patterns in arid catchments in the Negev Desert of Israel

机译:以色列内盖夫沙漠干旱集水区的动态水再分配模式建模

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In and climate regions, redistribution of runoff water is highly relevant for vegetation development. The process of water redistribution at catchment scale is studied with the landscape process model LAPSUS, mainly used for erosion and sedimentation modelling. LAPSUS, formerly applied in Mediterranean climates, is modified to deal with the arid climate of the Negev Desert of Israel. Daily event based model runs were used instead of yearly model runs, and the infiltration module was modified to better represent the spatial diversity in water availability in an and catchment. The model is calibrated for two small catchments in the Negev Desert of Israel, Halluqim and Avdat. First, a sensitivity analysis of the modified LAPSUS is performed. Pore volume appears to have an especially strong influence on the modelling results. Second, the capability of LAPSUS to deal with varying surface characteristics is assessed by comparing the water redistribution patterns in the two catchments with field data. Simulation results demonstrate that the catchments respond very differently to precipitation. Water redistribution is larger in the dominantly bedrock covered Halluqim compared to the dominantly loess covered catchment of Avdat. Consequently, Halluqim has more positions with water accumulation than Avdat, and can sustain a larger vegetation cover, including Mediterranean species. Finally, the modelled infiltration patterns are compared with vegetation cover in the catchments. The results indicate that there is a broad agreement between infiltration and vegetation patterns, but locally there is a strong mismatch, indicating that some of the involved processes are still missing from the model. Copyright (c) 2007 John Wiley & Sons, Ltd.
机译:在气候区域,径流水的重新分配与植被的发展高度相关。利用景观过程模型LAPSUS研究了流域尺度上的水的再分配过程,该模型主要用于侵蚀和沉降模型。 LAPSUS以前用于地中海气候,现在经过修改以应对以色列内盖夫沙漠的干旱气候。使用基于每日事件的模型运行来代替年度模型运行,并且对渗透模块进行了修改,以更好地表示流域和集水区中水的空间多样性。该模型针对以色列的内盖夫沙漠中的两个小流域(哈卢钦和阿夫达特)进行了校准。首先,对改进的LAPSUS进行灵敏度分析。孔体积似乎对建模结果有特别强烈的影响。其次,通过将两个流域的水再分配模式与现场数据进行比较,评估了LAPSUS处理各种表面特征的能力。模拟结果表明,流域对降水的响应截然不同。与Avdat占优势的黄土覆盖集水区相比,占优势的基岩覆盖的Halluqim的水再分配更大。因此,Halluqim的积水位置比Avdat多,并且可以维持更大的植被覆盖,包括地中海物种。最后,将模拟的入渗模式与集水区的植被覆盖率进行比较。结果表明,入渗与植被格局之间存在广泛共识,但局部地区存在强烈的不匹配,表明该模型中仍缺少某些涉及的过程。版权所有(c)2007 John Wiley&Sons,Ltd.

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