Comparison of methods to calculate groundwater recharge for karst aquifers under a Mediterranean climateComparaison de méthodes de calcul de la recharge des eaux souterraines pour des aquifères karstiques sous climat méditerranéenComparación de métodos de cálculo de la recarga de acuíferos kársticos en condiciones climáticas mediterráneas地中海气候下岩溶含水层地下水补给计算方法的比较研究。Comparação de métodos para calcular a recarga de água subterrânea para aquíferos cársticos em um clima mediterrâneo

被引:0
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作者
P Hepach [1 ]
L Bresinsky [2 ]
M Sauter [3 ]
Y Livshitz [2 ]
I Engelhardt [4 ]
机构
[1] Technical University of Berlin,Hydrogeology Department
[2] University of Göttingen,Geoscience Center
[3] University of Kassel,Institute for Water, Waste, Environment (IWAU)
[4] Hydrological Service of Israel,undefined
[5] Israel Water Authority,undefined
关键词
Israel; Palestine; Karst; Recharge; Unsaturated zone;
D O I
10.1007/s10040-024-02809-8
中图分类号
学科分类号
摘要
Karst aquifers can be particularly vulnerable to human activities and climate change due to their relatively high degree of connection with the surface. This study utilized an ensemble of event-based recharge calculation methods to address the problem of structural uncertainty for the example of the Western Mountain Aquifer (WMA), a Mediterranean karst aquifer located in Israel and the West Bank. Spatially distributed recharge estimates derived from the Soil and Water Assessment Tool (SWAT) and the process-based infiltration model (PIM) were compared to site-specific, empirical regression models. The SWAT and PIM mean annual recharge estimates ranged from 32–34.6% of precipitation, almost equating to the results of empirical regression models (32–36%). Future recharge predictions under the influence of climate change were quantified by parameterizing the SWAT and PIM methods with a downscaled regional climate model of Israel. SWAT predicts a 23% decrease in recharge by 2051–2070 relative to 1981–2001. In contrast, PIM shows a 9% decrease, possibly due to the representation of infiltration through preferential flow pathways and exclusion of surface runoff processes. These divergent projections underline key methodological differences in the representation of hydrological processes. Nevertheless, both methods effectively provided good estimates of groundwater recharge. The recharge rates estimated from the various methods were integrated into MODFLOW to assess their relative impacts on groundwater storage dynamics. The ensemble of MODFLOW projected groundwater storage outputs can provide guidance for sustainable groundwater management in the region.
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页码:1377 / 1396
页数:19
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