Climatic Modeling of Seawater Intrusion in Coastal Aquifers: Understanding the Climate Change Impacts

A. Lyra, A. Loukas, P. Sidiropoulos, N. Mylopoulos
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Abstract

The study examines the impacts of climate change and sea level rise on coastal aquifers, focusing on the influence of the components of the water cycle on seawater intrusion, and the evolution of the phenomenon in the future. The simulation of coastal water resources was performed using an integrated modeling system (IMS), designed for agricultural coastal watersheds, which consists of inter-connected models of surface hydrology (UTHBAL), groundwater hydrology (MODFLOW), and seawater intrusion (SEAWAT). Climatic models for the adverse impact scenario (RCP8.5) and the medium impact scenario (RCP4.5) of climate change were used. Transient boundary head conditions were set to the coastal boundary, to dynamically represent the rise in sea level due to climate change. The response of groundwater in the coastal Almyros Basin, located in central Greece, was simulated from 1991 to 2100. The findings indicate that seawater intrusion will be advanced in the future, in both climate change scenarios. The models show varying patterns in groundwater recharge, with varying uncertainty projected into the future, and sensitivity to time in the fluctuation of the components of the water cycle.
沿海含水层海水入侵气候模型:了解气候变化的影响
这项研究探讨了气候变化和海平面上升对沿海含水层的影响,重点是水循环各组成 部分对海水入侵的影响以及这种现象在未来的演变。对沿海水资源的模拟采用了专为沿海农业流域设计的综合建模系统(IMS),该系统 由相互连接的地表水文模型(UTHBAL)、地下水文模型(MODFLOW)和海水入侵模型 (SEAWAT)组成。采用了不利影响情景(RCP8.5)和中等影响情景(RCP4.5)的气候变化模型。在沿岸边界设置了瞬态边界水头条件,以动态表示气候变化引起的海平面上升。模拟了希腊中部沿海阿尔米罗斯盆地地下水从 1991 年到 2100 年的变化情况。研究结果表明,在两种气候变化情况下,海水入侵在未来都将加剧。模型显示了地下水补给的不同模式,对未来的预测具有不同的不确定性,以及水循环组成部分的波动对时间的敏感性。
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