• ▶ 2008-2024年被中国情报信息研究所评价中心评为“中国科技核心期刊”
  • ▶ 2019-2024年连续三届被中国科学院文献情报中心中国科学引文数据库CSCD(核心库)收录
  • ▶ 2021、2023年入编北京大学图书馆《中文核心期刊要目总览》
  • ▶ 2020-2024连续四年入选《科技期刊世界影响力指数(WJCI)报告》
孙永寿, 段水强, 李 燕, 曹广超.近年来青海三江源区河川径流变化特征及趋势分析水资源与水工程学报[J].,2015,26(1):52-57
近年来青海三江源区河川径流变化特征及趋势分析
Variation characteristics and trend analysis of runoff at the source regions of the three river in Qinghai during recent years
  
DOI:10.11705/j.issn.1672-643X.2015.01.010
中文关键词:  河川径流量  径流变化  集中度  集中期  生态保护  青海三江源
英文关键词:river runoff  runoff variation  concentration rate  concentration period  ecological protection  the source regions of the three river of Qinghai Province
基金项目:国家自然科学基金项目(41261004)
作者单位
孙永寿1, 段水强1, 李 燕1, 曹广超2 (1.青海省水文水资源勘测局 青海 西宁 810001 2.青海师范大学 青海省自然地理与环境过程重点实验室 青海 西宁 810008) 
摘要点击次数: 2080
全文下载次数: 1310
中文摘要:
      依据三江源区1956-2012年57年水文监测资料,采用距平分析,集中度、集中期、不均匀系数等方法,分析了自2005年青海三江源生态保护工程实施以来,三江源区河川径流变化特征及趋势。结果表明:三江源区2005-2012年系列径流的空间分布特征是由南向北递减;2005-2012年径流距平自东南向西北逐渐增大,最大为长江源头区,距平在80%以上,最小为源区东南部地区,距平在-10%左右;2005-2012年长江、澜沧江、黄河吉迈以上径流集中度、不均匀系数呈减小趋势,集中期有所推后,说明径流的年内分配趋于均匀、最大水量出现时间有所滞后;2005-2012年期间源区径流总体呈偏丰状态,各站径流较多年均值有明显增加;1956-2012年期间,长江源区径流有明显上升趋势,澜沧江、黄河源区径流无明显上升或下降趋势。
英文摘要:
      According to hydrological surveying data of 57 years of from 1956 to 2012, this paper used the methods such as dist anc average analysis, concentration rate, concentration period, coefficient of uniformity to analyze runoff variation feature and trend of the source regions of the three river since the ecological protection project wasimplemented in 2005. The results showed that space runoff distribution of the source regions of the three river increased from south to north from 2005 to 2012; distance average of runoff decreased from southeast to northwest from 2005 to 2012, the maximum was in source area of the Yangtze River, distance average was more than 80%, the minimum was in source area in southeastern regions, distance average was in about 10%; the runoff concentration rate, coefficient of uniformity presented decreasing trend, and the concentration period was delayed. The source area runoff was in overall wet station from 2005 to 2012. The runoff of each station has significantly increase more than annual average. The runoff has clear upward trend in Yangtze River, and has no significant upward or downward trend in the Lancang River and the Yellow River source region during 1956 to 2012.
查看全文  查看/发表评论  下载PDF阅读器
关闭