人民长江 ›› 2021, Vol. 52 ›› Issue (8): 84-91.doi: 10.16232/j.cnki.1001-4179.2021.08.013

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基于极点对称模态分解的三江源径流时空演变规律

李凯,任卓钰,王永强, 许继军   

  • 发布日期:2021-09-27

Spatial-temporal evolution of runoff based on extreme-point symmetric mode decomposition in Three-River Headwaters Region

LI Kai, REN Zhuoyu ,WANG Yongqiang, XU Jijun   

  • Published:2021-09-27

摘要: 气候变化和人类活动加剧改变了地球的水循环系统,因此,重新认识和掌握流域水循环演变规律具有重要意义。利用极点对称模态分解(ESMD)方法同时从趋势、突变、周期3个方面对三江源径流变化进行分析,并与现有的检测方法进行对比。结果表明:(1)黄河源地区由于降水增加趋势不明显,随着气温升高,蒸散量增大,导致年径流呈现不显著的下降趋势;长江源、澜沧江源径流由于降水和冰川融雪的增加,导致年径流呈现显著增强的趋势。(2)黄河源近61 a的径流过程在1990~1994年、2008年左右发生明显突变,长江源径流过程在2006年左右发生显著突变,澜沧江源径流过程在20世纪90年代和2008年左右发生突变。(3)黄河源近61 a径流过程存在12~15 a和30 a的周期性变化;长江源近60 a径流过程存在13~15 a的周期性变化;澜沧江源近49 a径流过程存在15~16 a和28 a的周期性变化,这些周期性变化主导着三江源年径流变化特性。

关键词: 径流变化; 周期分析; 气候变化; 极点对称模态分解; 长江; 黄河; 澜沧江;

Abstract: Climate change and the strengthening of human activities have influenced the earth's water cycle system.Therefore, it is of great significance to re-understand and master the evolution of water cycle in the basin.We use the extreme-point symmetric mode decomposition(ESMD) method to analyze the runoff variation in the Three-River Headwaters Region from aspects of trend, sudden change, and cycle, and compare the ESMD with existing detection methods.The results showed that:(1) in the source region of the Yellow River, the increasing trend of precipitation was not obvious and the evapotranspiration increased as the temperature increased, which resulted in an insignificant downward trend of annual runoff.The annual runoff in the source region of the Changjiang River and the Lancang River increased significantly due to the increase of precipitation and glacial snow melting.(2) The 61 years runoff process of the Yellow River source region experienced significantly abrupt changes between 1990~1994 and around 2008.The runoff process of the Changjiang River source region experienced significantly abrupt change around 2006.The runoff process of the Lancang River source region had an abrupt changes in the 1990 s and around 2008.The 61-years runoff process of the Yellow River source region had cyclic variation of 12~15 a and 30 a.The 60-years runoff process of the Changjiang River source region had 13~15 a cyclic variation.The 49-years runoff process of the Lancang River source region had cyclical changes of 15~16 a and 28 a.And these cyclical changes dominate the characteristics of the annual runoff variation of the Three-River Headwaters Region.

Key words: runoff variation; cycle analysis; climate change; ESMD; Changjiang River; Yellow River; Lancang River;