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Coupled modeling approach to assess climate change impacts on groundwater recharge and adaptation in arid areas : Coupled modeling approach to assess climate change impacts on groundwater recharge

机译:评估气候变化对干旱地区地下水补给和适应的影响的耦合建模方法:评估气候变化对地下水补给影响的耦合模拟方法

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摘要

The effect of future climate scenarios on surface and groundwater resources was simulated using a model- ing approach for an artificial recharge area in arid southern Iran. Future climate data for the periods of 2010–2030 and 2030–2050 were acquired from the Canadian Global Coupled Model (CGCM 3.1) for scenarios A1B, A2, and B1. These scenarios were adapted to the studied region us- ing the delta-change method. A conceptual rainfall–runoff model (Qbox) was used to simulate runoff in a flash flood prone catchment. The model was calibrated and validated for the period 2002–2011 using daily discharge data. The projected climate variables were used to simulate future runoff. The rainfall–runoff model was then coupled to a calibrated groundwater flow and recharge model (MODFLOW) to simulate future recharge and groundwater hydraulic heads. As a result of the rainfall–runoff modeling, under the B1 scenario the number of floods is projected to slightly increase in the area. This in turn calls for proper management, as this is the only source of fresh water supply in the studied region. The results of the groundwater recharge modeling showed no significant difference between present and future recharge for all scenarios. Owing to that, four abstraction and recharge scenarios were assumed to simulate the groundwater level and recharge amount in the studied aquifer. The results showed that the abstraction scenarios have the most substantial effect on the groundwater level and the continuation of current pumping rate would lead to a groundwater decline by 18 m up to 2050.
机译:伊朗南部干旱地区的人工补给区采用建模方法模拟了未来气候情景对地表和地下水资源的影响。从场景A1B,A2和B1的加拿大全球耦合模型(CGCM 3.1)获取了2010-2030年和2030-2050年的未来气候数据。这些情况通过德尔塔变化法适应了研究区域。使用概念性降雨-径流模型(Qbox)来模拟山洪易发地区的径流。使用每日排放数据对2002-2011年期间的模型进行了校准和验证。预计的气候变量用于模拟未来径流。然后将降雨径流模型与校准后的地下水流量和补给模型(MODFLOW)耦合,以模拟将来的补给和地下水水头。作为降雨径流模型的结果,在B1情景下,预计该地区的洪水数量将略有增加。反过来,这也要求适当的管理,因为这是所研究地区唯一的淡水供应来源。地下水补给模型的结果表明,在所有情况下,当前补给与未来补给之间都没有显着差异。因此,假设采用四种取水和补给情景来模拟所研究含水层中的地下水位和补给量。结果表明,取水方案对地下水位的影响最大,到2050年,持续抽水将导致地下水下降18 m。

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