首页|气候变化和人类活动对滹沱河上游流域水文干旱演变的影响

气候变化和人类活动对滹沱河上游流域水文干旱演变的影响

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基于滹沱河上游流域1961-2018年逐月径流数据和逐日气象数据,采用ABCD水文模型和以时间为解释变量的GAMLSS模型,构建时变标准化径流指数,综合考虑变点分析、气候变化和社会发展的不同阶段,将研究时域划分为自然期(1961-1979年)、影响期1(1980-1997年)和影响期2(1998-2018年)3个阶段,进而基于干旱指数关于时间的线性变化率量化气候变化和人类活动对非平稳水文干旱演变的影响。结果表明:在2个影响期的四季和年尺度上,非平稳水文干旱均表现为缓解趋势;在影响期1,气候变化和人类活动在季和年尺度上均以缓解水文干旱为主,但人类活动以53。22%~89。11%的贡献率占主导地位;在影响期2的四季和年尺度上,气候变化以50。72%~72。68%的贡献率主导了水文干旱的缓解趋势,而人类活动则以-49。27%~-27。32%的贡献率加剧了水文干旱;人类活动与气候变化导致的干旱指数序列在影响期2的3个月和12个月尺度下均呈现出显著负相关,这说明进入21世纪之后,人们对水循环的干预较20世纪更科学合理。
Climate changes and human activities affect evolution of hydrological droughts in the upper watershed of Hutuo River
Monthly runoff data and daily meteorological data in the upper reaches of Hutuo River from 1961-2018 were subject to analysis with the ABCD hydrological model and GAMLSS model,to calculate time-varying standardized runoff index.Change point analysis,climate changes and different stages of social development were considered,with the study time domain divided into three phases:natural period(1961-1979),first impact period(1980-1997)and second impact period(1998-2018).Influence of climate changes and human activities on evolution of non-stationary hydrological drought under changing environment were quantified,based on linear rate of change of drought index with respect to time.On seasonal and annual scales of the two influence periods,trend of non-stationary hydrological drought was all alleviated.In the first impact period,climate changes and human activities mainly alleviated hydrological drought on both seasonal and annual scales,but human activities dominated contribution rate at 53.22%-89.11%.On seasonal and annual scales of the second influence period,main factor of hydrological drought mitigation was climate changes,with contributions at 50.72%-72.68%.However,hydrological drought was exacerbated by human activities,contributing from-49.27%to-27.32%.In the second influence period,drought index series caused by human activities and climate changes showed a significant negative correlation on both 3-month scale and 12-month scale.This work indicates that after entering the 21st century,people's intervention in the water cycle is more scientific and rational than in the 20th century.

climate changeshuman activitiesGAMLSSHutuo Riverdrought

苗正伟、刘璐

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河北水利电力学院水利工程系,河北沧州

气候变化 人类活动 GAMLSS 滹沱河 干旱

2024

北京师范大学学报(自然科学版)
北京师范大学

北京师范大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.505
ISSN:0476-0301
年,卷(期):2024.60(6)