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人类活动下吉泰盆地典型流域水文干旱多要素响应特征

孙可可 姚立强 刘雁翼 张秀平 吴涛

长江科学院院报2026,Vol.43Issue(5):32-41,10.
长江科学院院报2026,Vol.43Issue(5):32-41,10.DOI:10.11988/ckyyb.20250384

人类活动下吉泰盆地典型流域水文干旱多要素响应特征

Responses of Multiple Elements to Hydrological Drought Driven by Human Activities in Typical Watersheds of Jitai Basin

孙可可 1姚立强 1刘雁翼 2张秀平 3吴涛2

作者信息

  • 1. 长江科学院水资源综合利用研究所,武汉 430010||长江科学院水利部长江重点实验室,武汉 430010
  • 2. 中铁水利水电规划设计集团有限公司规划院,南昌 330029
  • 3. 江西省水利科学院江西省鄱阳湖流域生态水利技术创新中心,南昌 330029
  • 折叠

摘要

Abstract

[Objective]This study aims to investigate the differentiated effects of various driving factors on the stage-specific characteristics of hydrological drought in the Jitai Basin under the influence of climate change and in-tensive human activities.[Methods]We collected meteorological and hydrological data from 1959 to 2023 from three typical watersheds(the Shushui,Wujiang,and Tongjiang Rivers)in the Jitai Basin,and adopted the Pettitt test to divide the study period into a baseline period,a transition period,and a change period.By using the im-proved two-parameter monthly water balance model,we analyzed the drought characteristics and the quantitative effects of driving factors in each stage,and clarified the dominant role of different driving factors as well as their nonlinear regulation mechanisms.[Results]1)The runoff generation mechanisms of the three typical watersheds shifted around 1980 and 2008.Specifically,in baseline period(1959-1980),the underlying surface conditions of the watersheds were relatively stable,hydrological processes were dominated by natural climate drivers,and runoff variations were directly controlled by the precipitation-evaporation balance,with no obvious disturbance from human activities.In transition period(1981-2008),the intensifying regional human activities began to alter the original runoff generation mechanisms of the watersheds.In the change period(2009-2023),underlying surface modifica-tion and water conservancy project regulation became dominant factors.The runoff coefficient α increased signifi-cantly in transition period and then declined in the change period,which also indicated that the regulatory intensity of human activities on runoff exceeded natural fluctuations.In terms of drought characteristic variations,drought se-verity and duration decreased notably in the transition period compared with the baseline period,but rebounded in the change period;the average drought severity of the three typical watersheds increased by 46.2%,26.9%and 25.9%respectively relative to the transition period.2)By introducing a regulating coefficient of parameter C during wet and dry periods,the improved two-parameter monthly water balance model effectively improved the overall sim-ulation accuracy of runoff series,especially for low-flow and drought months.The Nash-Sutcliffe efficiency coeffi-cient(NSE)was higher than 0.7 and the correlation coefficient R exceeded 0.85 in both the baseline and transition periods,with the water balance error controlled within±1%.In the change period,the measured runoff series was heavily disturbed by human activities,which increased the difficulty of simulating monthly-scale runoff series.Pa-rameter calibration results showed that the value of C for each typical watershed in transition period was lower than that in baseline period,but rebounded in the change period,reflecting regular variations in the precipitation-evapo-ration relationship of the watersheds across different stages.High temperature and low rainfall in summer and au-tumn were critical driving factors of hydrological drought in the Jitai Basin,with strong sensitivity to drought severi-ty.A 10%reduction in precipitation during this period led to an increase of 0.14-0.23 in drought severity,accom-panied by a marginally diminishing effect.Nevertheless,compared with the baseline period,human activities played a dominant role in the change period,causing greater variations in runoff depth and drought severity than climate change factors.[Conclusion]The multi-stage quantitative method for driving factors constructed in this study reveals the nonlinear regulatory effects of climate change and human activities on hydrological drought severity in the Jitai Basin at different stages,clarifies the influence intensity,sensitivity and stage characteristics of each driving factor,and identifies the nonlinear regulation of these factors on drought severity.

关键词

水文干旱/吉泰盆地/人类活动影响/两参数月水量平衡模型/干旱烈度

Key words

hydrological drought/Jitai Basin/effects of human activities/two-parameter monthly water balance model/drought severity

分类

天文与地球科学

引用本文复制引用

孙可可,姚立强,刘雁翼,张秀平,吴涛..人类活动下吉泰盆地典型流域水文干旱多要素响应特征[J].长江科学院院报,2026,43(5):32-41,10.

基金项目

中国中铁股份有限公司科技研究开发计划项目(2022-重大-08) (2022-重大-08)

江西省技术创新引导类计划项目(2023KSG01005) (2023KSG01005)

长江科学院院报

1001-5485

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