Using hydrological modeling and satellite observations to elucidate subsurface and surface hydrological responses to the extreme drought

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Journal of Hydrology Pub Date : 2024-10-17 DOI:10.1016/j.jhydrol.2024.132174
Zixuan Tang , Yongqiang Zhang , Jing Tian , Ning Ma , Xiaojie Li , Dongdong Kong , Yijing Cao , Xuening Yang , Longhao Wang , Xuanze Zhang , Yuyin Chen
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Abstract

Climate change and anthropogenic activities have intensified extreme weather events globally. In the summer of 2022, the Yangtze River Basin (YRB) in China experienced an extreme drought, significantly impacting the ecosystems and society. However, the specific effects of this extreme drought on surface and subsurface hydrological dynamics remain unclear. Here we employed satellite-observed terrestrial water storage anomaly (TWSA) and a modified hydrological model with consideration of reservoir operation, human water consumption, and water diversion engineering to quantify how subsurface and surface water in YRB responded to such an extreme drought in 2022. Validation against a series of observations shows that the modified model has good performance in reproducing daily streamflow, reservoir water storage, lake water storage, and snow water equivalent. It achieved more precise GRACE TWSA estimates in the YRB with significant human intervention, and therefore it can accurately quantify both surface and subsurface hydrological responses to the 2022 extreme drought. Compared to the same months (July-December) in 2015–2021, the drought in 2022 resulted in a decrease in precipitation and discharge of 373 km3 (36 %) and 324 km3 (50 %), respectively, while an increase in evapotranspiration of 156 km3 (29 %) in the YRB. In general, the surface water storage (SWS) is relatively low from July 2022, followed by subsurface water storage (SSWS) from August 2022, indicating an approximately one-month lag from the former to the latter. During the latter half year of 2022, the SWS and SSWS reduced by 48 km3 and 83 km3, respectively, suggesting the changes in the latter dominated the TWS variations. This study sheds light on the responses of surface and subsurface hydrology to extreme droughts, and the hydrological modeling framework with consideration of human activities proposed here holds applicability beyond the YRB.
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利用水文模型和卫星观测来阐明地下和地表水文对极端干旱的反应
气候变化和人为活动加剧了全球极端天气事件。2022 年夏季,中国长江流域遭遇特大干旱,对生态系统和社会造成了严重影响。然而,这次特大干旱对地表和地下水文动态的具体影响仍不清楚。在此,我们利用卫星观测到的陆地蓄水异常(TWSA)和一个考虑了水库运行、人类用水和引水工程的改进水文模型,量化了 2022 年长江流域地下水和地表水如何应对这场特大干旱。根据一系列观测数据进行的验证表明,改进后的模型在再现日径流量、水库蓄水量、湖泊蓄水量和雪水当量方面具有良好的性能。在大量人工干预的情况下,该模型在YRB中实现了更精确的GRACE TWSA估算,因此可以准确量化地表和地下水对2022年极端干旱的响应。与 2015-2021 年的相同月份(7 月至 12 月)相比,2022 年的干旱导致 YRB 的降水量和排水量分别减少了 373 千立方米(36%)和 324 千立方米(50%),而蒸散量增加了 156 千立方米(29%)。总体而言,从 2022 年 7 月开始,地表蓄水量(SWS)相对较低,从 2022 年 8 月开始,地表下蓄水量(SSWS)紧随其后,这表明从前者到后者有大约一个月的滞后期。在 2022 年的后半年,地下蓄水量和地下水储量分别减少了 48 千立方米和 83 千立方米,表明后者的变化主导了总温差变化。这项研究揭示了地表和地下水文对极端干旱的响应,本文提出的考虑人类活动的水文建模框架适用于长三角地区以外的地区。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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