水科学进展2024,Vol.35Issue(2) :313-324.DOI:10.14042/j.cnki.32.1309.2024.02.012

环境变化对澜沧江出境水文过程变异的影响

Impact of environmental changes on variability of outlet hydrological process of the Lancang River basin

王乐扬 张建云 宁忠瑞 贾雨凡 孙高霞 王国庆
水科学进展2024,Vol.35Issue(2) :313-324.DOI:10.14042/j.cnki.32.1309.2024.02.012

环境变化对澜沧江出境水文过程变异的影响

Impact of environmental changes on variability of outlet hydrological process of the Lancang River basin

王乐扬 1张建云 2宁忠瑞 3贾雨凡 3孙高霞 4王国庆4
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作者信息

  • 1. 河海大学水文水资源学院, 江苏 南京 210098;长江保护与绿色发展研究院, 江苏 南京 210098
  • 2. 长江保护与绿色发展研究院, 江苏 南京 210098;南京水利科学研究院水灾害防御全国重点实验室, 江苏 南京 210029
  • 3. 长江保护与绿色发展研究院, 江苏 南京 210098;河海大学水安全与水科学协同创新中心,江苏 南京 210098
  • 4. 南京水利科学研究院水灾害防御全国重点实验室, 江苏 南京 210029;水利部应对气候变化研究中心, 江苏 南京 210029
  • 折叠

摘要

变化环境改变河流水文节律,影响流域水资源的开发利用;澜沧江-湄公河是位于东南亚源于中国西南的跨境河流,科学厘清澜沧江径流变化原因是实现澜沧江-湄公河流域跨境水利益共享的重要基础工作.基于 1961-2020 年允景洪水文站的实测径流量资料,采用数理统计与水文模拟相结合的研究途径,诊断径流序列的变异特征,定量分析气候变化和人类活动对径流及其年内分配的影响.结果表明:①1961-2020 年允景洪站实测年径流量呈显著性减少趋势,其中,1-5 月径流量呈增加趋势,6-12 月径流量呈减少趋势;实测年径流量在 2008 年发生突变.② RCCC-WBM模型能够较好地模拟基准期(1961-2008 年)的天然径流量过程,模拟相对误差小于1%;模拟的人类活动影响期间(2009-2020 年)天然径流量约为 371.8 mm,较基准期偏少 6.8%,这是气候变化引起的.③ 水利工程建设运行是澜沧江最主要的人类活动,是水库蓄水运行期(2009-2013 年)径流减少的主要原因;气候变化对水库稳定正常运行期(2014-2020 年)径流减少贡献更大,约为 61.7%.④ 水库运行调度使得 2014-2020年汛期(6-11 月)径流量减少44.3%,非汛期(12 月至翌年 5 月)径流量增加 134.3%;澜沧江干流水库对径流的削峰补枯调节作用在一定程度上保障了湄公河中下游的防洪安全与供水安全.

Abstract

Environment change alters hydrological rhythms and affects utilization of water resources for a river basin.The Lancang-Mekong River is a transboundary river in Southeast Asia originated in the Southwestern China.It is of significance to scientifically quantifying runoff change attribution of the Langcang River for supporting water benefits share between countries which the Lancang-Mekong River runs across.Based on the recorded runoff data series from 1961 to 2020 gauged at the Yunjinghong hydrometric station on the Langcang River,the variability characteristics of runoff series and the impact of climate change and human activities on runoff change as well as its seasonal distribution were investigated by using statistical methods and hydrological simulation methods.The results show that:① The measured annual runoff at Yunjinghong station showed a significant decrease trend from 1961 to 2020,with an increase in runoff during the period from January to May and a decrease in runoff in period from June to December.The abrupt change of the measured annual runoff series was occurred in 2008.② The RCCC-WBM model performs well for monthly natural discharge simulation in the baseline period of 1961-2008 with relative error of less than 1.0%.The simulated natural annual runoff in the human-disturbance period of 2009-2020 is about 371.8 mm,which is 6.8%less than that in baseline period.The reduction is induced by climate change.③ Reservoirs construction and operation is the utmost human activity in the Langcang River.Human activities are the main reason of runoff decrease in the reservoir impoundment period of 2009-2013,while climate change is principal driver of runoff reduction in in the reservoir operation period of 2014-2020,which contribution is about 61.7%of total runoff reduction.④ The reservoirs operation makes runoff decrease by 44.3%in flood season from June to November and increase by 134.3%in dry season from December to May for period of 2014-2020.The regulation function of reservoirs on the Langcang River for decreasing flood discharge and increasing low flow has been guaranteeing security of water supply and flood control for the middle and lower reaches of the Mekong River.

关键词

气候变化/人类活动/径流量/RCCC-WBM模型/归因识别/澜沧江流域

Key words

climate change/human activities/runoff/RCCC-WBM model/attribution analysis on runoff change/Lancang River basin

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基金项目

国家自然科学基金(92047301)

国家自然科学基金(52121006)

出版年

2024
水科学进展
南京水利科学研究院 水利部 交通运输部 国家能源局 中国水利学会

水科学进展

CSTPCDCSCD北大核心
影响因子:1.931
ISSN:1001-6791
被引量1
参考文献量39
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