历年降水的地下蓄积有助于缓解旱地木本盆地水分亏余

IF 6.3 1区 地球科学 Q1 ENGINEERING, CIVIL
Zongxu Yu , Ping Wang , Jingjie Yu , Tianye Wang
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引用次数: 0

摘要

了解旱地地下水与植被之间错综复杂的关系对保护生态健康至关重要,特别是在干旱的中亚内陆河流域。然而,流域地下水在植被亏盈时的缓解机制尚不清楚,这限制了我们对旱地维持生态系统稳定功能的认识。这项研究的目的是在中亚最大的内陆河之一阿姆河(AD)沿岸的子流域内弥合这一知识差距。利用气象水文资料和木本植被总初级生产力(GPP)资料,评价了1982 - 2018年旱地生长季(GS)亏余的储存量地下水(S)缓解程度。采用非参数Spearman相关系数、偏相关分析和多元线性回归方法,分别计算了苗期降水对地下储水量的变化趋势、植被对不同水分条件的响应以及水分亏缺和富余情况下地下储水量的缓解能力。结果表明,下游子流域有PGS降水的倾向,S和GPP对标准化降水蒸散指数(SPEI)在6个月和12个月的时间尺度上均表现出较强的响应。前一年随机降水S有效地解释了PGS和GS之间在水分亏缺或富余对植被影响下的水携带缓解作用。在气象条件日趋干旱的AD子流域,S水量虽逐年减少,但仍将成为缓解水资源压力和生态危机的重要水源。该研究对维持内陆河流域生态稳定提供了更深入的认识,有助于为气候变化条件下的灾害防治提供解决方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Subsurface storage of previous year’s precipitation contributes to mitigating water deficit and surplus in dryland woody basin

Subsurface storage of previous year’s precipitation contributes to mitigating water deficit and surplus in dryland woody basin
Understanding the intricacies of the relationships between subsurface water and vegetation in drylands is of paramount importance for preserving the ecological well-being, especially in arid Central Asian endorheic basins. However, the mitigation mechanism of subsurface water in the basin when vegetation encounters water deficit or surplus remains unclear, which limits our understanding of dryland function in maintaining ecosystem stability. This study aimed to bridge this knowledge gap within the sub-basins along Amu Darya (AD), one of the largest inland rivers in Central Asia. The extent of stored subsurface water (S) mitigation for the growing season (GS) water deficit and surplus from 1982 to 2018 was evaluated using the meteoro-hydrological data and woody vegetation Gross Primary Productivity (GPP) data. The nonparametric Spearman correlation coefficient, partial correlation analysis, and multiple linear regression method were employed to calculate the tendency of precipitation during pre-growing season (PGS) for subsurface storage, the response of vegetation to varying water conditions, and the mitigating capacity of subsurface water storage under water deficit and surplus situations, respectively. Our results showed that the downstream sub-basins tended to store PGS precipitation, and both S and GPP exhibited strong responses to the Standardized Precipitation Evapotranspiration Index (SPEI) on both 6- and 12-month timescales. The S from the previous year’s random precipitation effectively explained the mitigating effect of water carryover between the PGS and GS under the impact of water deficit or surplus on vegetation. In the AD sub-basins where the meteorological conditions are gradually becoming more arid, the S will become an important water source to mitigate water stress and ecological crises, despite its decreasing volume year by year. The study provides deeper insight into maintaining ecological stability in the endorheic basin, which will help provide solutions for disaster prevention under the conditions of climate change.
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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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