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Impacts of surface and groundwater variability response to future climate change scenarios in a large Mediterranean watershed

机译:地中海大流域地表和地下水变化对未来气候变化情景的影响

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The objective of this research was to better understand the dynamics of surface-groundwater interactions in a large Mediterranean watershed (Evrotas River Basin) and to improve the seasonal forecasting of a potential hydrological drought under future climate change scenarios. This is achieved by integrating the quasi-distributed watershed Soil and Water Assessment Tool (SWAT) model with the three-dimensional groundwater flow Princeton Transport Code (PTC) model. The combined models are applied to the alluvial plain of Evrotas watershed in Greece by considering the interaction between the stream network and the aquifer to better spatially represent feedback fluxes within the surface and groundwater domains. Model simulation (2007-2011) was in good agreement with field observations demonstrating that this integrated modeling approach provides a more realistic representation of the water exchanges between surface and subsurface domains and constrains more the calibration with the use of both surface and subsurface observed data. Finally, the integrated SWAT-PTC model was used to study the impact of future climate change on surface and groundwater resources of the area under three different climate change scenarios. The results indicate that the study area is very sensitive to potential future climate changes. Upstream reaches display a loss of surface water to underlying groundwater systems whereas downstream the main river receives recharge from groundwater as the water table approached the surface topography. The low flow characterization for the current situation shows that a large part of the stream network will be too dry to accommodate the development of a viable aquatic ecological community throughout the years. In dry periods, the amount of water that is supplied to the aquifer is 40.9% less than the amount of water that is supplied under current climate conditions highlighting the need for new management strategies that must be implemented in order to avoid setbacks in the allocation of water resources in the future.
机译:这项研究的目的是更好地了解一个大型地中海流域(埃夫罗塔斯河流域)的地表水相互作用,并改进未来气候变化情景下潜在水文干旱的季节预报。这是通过将准分布式流域土壤和水评估工具(SWAT)模型与三维地下水流普林斯顿运输代码(PTC)模型集成而实现的。通过考虑河流网络和含水层之间的相互作用,将组合模型应用于希腊Evrotas流域的冲积平原,以更好地空间表示地表水域和地下水域内的反馈通量。模型仿真(2007-2011年)与现场观察结果非常吻合,表明这种集成的建模方法可以更真实地表示地表和地下区域之间的水交换,并通过使用地表和地下观测数据来约束更多的校准。最后,使用集成的SWAT-PTC模型研究了三种不同气候变化情景下未来气候变化对该地区地表和地下水资源的影响。结果表明,研究区域对潜在的未来气候变化非常敏感。上游河段向地下地下水系统流失了地表水,而下游主干河则随着地下水位接近地表地形而从地下水中补给水。当前状况的低流量特征表明,河网的很大一部分将太干燥,无法容纳多年来可持续的水生生态社区的发展。在干旱时期,向含水层供应的水量比在当前气候条件下供应的水量少40.9%,这突显了对新管理策略的需求,必须采取新的管理策略,以避免在分配水资源方面受到挫折。未来的水资源。

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