Impact of climate change on permanent lakes in a semiarid region: Southwestern Mediterranean basin (S Spain)

IF 8 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
A. Jiménez-Bonilla , M. Rodríguez-Rodríguez , J.L. Yanes , F. Gázquez
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Abstract

In recent decades, many wetlands in the Mediterranean watershed have dried up. We forecast the impact of climate change on the hydrology of three permanent lakes in a semiarid areo of the southwestern Mediterranean region. To achieve this, we applied daily water balance models to calculate variations in water levels and validated our approach using actual lake level measurements spanning over 20 years. To delve into groundwater/lake interactions, we calculated several hydrological indices and compared evaporation with the water level drop during extremely dry periods. After validating the three hydrological models, we applied the RCP 4.5 and RCP 8.5 climate change scenarios. We found Zóñar Lake highly resilient to climate changes because of groundwater contributions, resulting in minimal lake level oscillations even during periods of low rainfall. However, spring management and/or groundwater extractions may affect the lake hydroperiod. The Amarga and Grande lakes have weaker lake/groundwater interactions and show significant water lake level fluctuations, making them more sensitive to climate change. Indeed, our model predict that these lakes will transition into semipermanent or seasonal playa-lakes by mid-21th century. We found that deep and spring and/or groundwater-fed lakes are less vulnerable to climate changes. These results highlight the importance of developing robust hydrogeological models in such water bodies, focusing on the climate changes vulnerability of wetlands in semiarid regions, in order to formulate an integrated strategy for water resources management.

Abstract Image

气候变化对半干旱区永久性湖泊的影响:地中海西南部盆地(西班牙南部)。
近几十年来,地中海流域的许多湿地已经干涸。本文预测了气候变化对地中海西南部半干旱区三个永久湖泊水文的影响。为了实现这一目标,我们应用每日水量平衡模型来计算水位的变化,并使用超过20年的实际湖泊水位测量来验证我们的方法。为了深入研究地下水与湖泊的相互作用,我们计算了几个水文指数,并比较了极端干旱时期的蒸发与水位下降。在验证了3种水文模型之后,我们应用了RCP 4.5和RCP 8.5气候变化情景。我们发现Zóñar湖对气候变化具有高度的弹性,因为地下水的贡献,即使在低降雨量期间,湖泊水位波动也很小。然而,泉水管理和/或地下水开采可能会影响湖泊水期。阿玛加湖和格兰德湖的湖/地下水相互作用较弱,水位波动明显,对气候变化更为敏感。事实上,我们的模型预测,到21世纪中期,这些湖泊将转变为半永久性或季节性的湖湖。我们发现深层湖泊、泉水湖泊和/或地下水湖泊不太容易受到气候变化的影响。这些结果强调了在这些水体中建立强大的水文地质模型的重要性,重点关注半干旱区湿地的气候变化脆弱性,以便制定水资源管理的综合战略。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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