A novel framework for assessing the joint and relative impacts of precipitation and groundwater on ecological drought processes in Northwest China

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-09-22 DOI:10.1002/hyp.15289
Tiangliang Jiang, Yanping Qu, Xiaoling Su, Jiangdong Chu, Yu Han
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Abstract

Ecological drought has emerged as a critical research topic within eco-hydrology, driven by the increased drought risk associated with global warming. This study aims to unravel the hydrological processes driving ecological drought in Northwest China by (1) constructing standardized indices for precipitation, groundwater storage anomaly, and ecological water deficit to detect variation across different hydrological components; (2) developing a framework to assess the joint and relative impacts of precipitation and groundwater variations on ecological drought; and (3) identifying the primary hydrological drivers of ecological drought across different regions. The results indicate that the joint impact of precipitation and groundwater on ecological drought variation dominates approximately 60% of the area, primarily in arid and semi-arid regions. The average contribution of this joint impact to the alleviation of ecological drought ranges between 0.26 and 0.43 across all seasons. Notably, groundwater scarcity, rather than precipitation variation, is the primary driver of ecological drought in regions such as southern Shaanxi, southeastern Gansu, and southern Qinghai, accounting for 12.7% to 21.8% of the total area. These insights into the complex hydrological processes underlying ecological drought have significant implications for water resource management and ecosystem conservation in drought-prone regions. This research provides valuable information for mitigating drought impacts and protecting vulnerable ecosystems in Northwest China and similar regions worldwide.

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评估降水和地下水对中国西北地区生态干旱过程的共同和相对影响的新框架
由于全球变暖导致干旱风险增加,生态干旱已成为生态水文学的一个重要研究课题。本研究旨在通过以下方法揭示驱动中国西北地区生态干旱的水文过程:(1)构建降水、地下水储量异常和生态缺水的标准化指数,以探测不同水文成分之间的变化;(2)建立评估降水和地下水变化对生态干旱的联合和相对影响的框架;以及(3)识别不同区域生态干旱的主要水文驱动因素。研究结果表明,降水和地下水对生态干旱变化的共同影响约占 60%,主要集中在干旱和半干旱地区。在所有季节,这种共同影响对缓解生态干旱的平均贡献率在 0.26 至 0.43 之间。值得注意的是,在陕西南部、甘肃东南部和青海南部等地区,地下水匮乏而非降水变化是生态干旱的主要驱动因素,占总面积的 12.7% 至 21.8%。这些关于生态干旱背后复杂水文过程的见解对干旱易发地区的水资源管理和生态系统保护具有重要意义。这项研究为减轻干旱影响和保护中国西北地区及全球类似地区脆弱的生态系统提供了宝贵的信息。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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