用户名: 密码: 验证码:
青海湖流域径流变化趋势及归因分析
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Trend and Attribution Analysis of Runoff in Qinghai Lake Basin
  • 作者:王欢 ; 刘九夫 ; 谢自银 ; 马乐军
  • 英文作者:WANG Huan;LIU Jiu-fu;XIE Zi-yin;MA Le-jun;State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute;Research Center for Climate Change,MWR;College of Hydrology and Water Resources,Hohai University;
  • 关键词:青海湖 ; 气温 ; 降水 ; 径流 ; 积雪面积
  • 英文关键词:Qinghai Lake;;temperature;;precipitation;;runoff;;snow cover area
  • 中文刊名:SDNY
  • 英文刊名:Water Resources and Power
  • 机构:南京水利科学研究院水文水资源与水利工程科学国家重点实验室;水利部应对气候变化研究中心;河海大学水文水资源学院;
  • 出版日期:2018-08-25
  • 出版单位:水电能源科学
  • 年:2018
  • 期:v.36;No.216
  • 基金:国家重点研发计划(2016YFC0401504);; 国家自然科学基金项目(91647111)
  • 语种:中文;
  • 页:SDNY201808005
  • 页数:5
  • CN:08
  • ISSN:42-1231/TK
  • 分类号:24-27+38
摘要
针对青海湖流域近年来径流量增加的现状,根据流域内1976~2016年水文、遥感观测数据,采用滑动平均法、Mann-Kendall趋势检验及突变检验法、距平累积法和双累积曲线法研究了流域气温、降水、径流及积雪等的时空特性。结果表明,青海湖流域气温总体变化呈上升趋势,并在1998年前后发生突变;1976~2016年气温上升率为0.06℃/a;流域内降水量呈缓慢上升,2014年后降水量显著增加。布哈河流域近5年冰雪覆盖面积缩小较迅速且入湖径流量上升趋势显著;通过径流影响因素分析,2005~2015年冻土及冰雪融化对径流影响占主导地位,达75%,降水量占25%。这说明青海湖流域正向暖湿化发展,近年来青海湖湖泊的扩张主要是由降水和径流增加所致。
        According to the hydrological and remote sensing data of 1976-2016 years in the Qinghai Lake Basin,the temporal and spatial characteristics of watershed temperature,precipitation,runoff and snow cover were studied by moving average method,Mann-Kendall trend test and mutation test,anomaly cumulative method and double cumulative curve method.The results indicate that the temperature of Qinghai Lake Basin changes in the overall upward trend,and mutated in 1998.The temperature rise rate during1976-2016 year is 0.06 C/a.The precipitation in the basin increased slowly,and the precipitation increased significantly after 2014.The ice covered area in Buha River Basin in recent 5 years is shrinking rapidly and runoff flow into the lake rise significantly.Through the analysis of the influencing factors of runoff,the 2005-2015 year permafrost and the melting of ice and snow have a dominant influence on the runoff,accounting for75%,and the amount of precipitation is 25%.The Qinghai Lake Basin is developing to the trend of warm and humid.In recent years,the expansion of Qinghai Lake is mainly caused by the increase of precipitation and runoff.
引文
[1]《中国河湖大典》编纂委员会.中国河湖大典.西北诸河卷[M].北京:中国水利水电出版社,2014.
    [2]Thompson L G,Mosley-Thompson E,Davis M E,et al.Tropical Glacier and Ice Core Evidence of Climate Change on Annual to Millennial Time Scales[J].Climatic Change,2003,59(1-2):137-155.
    [3]Bayard D,Sthli M,Parriaux A,et al.The Influence of Seasonally Frozen Soil on the Snowmelt Runoff at Two Alpine Sites in Southern Switzerland[J].Journal of Hydrology,2005,309(1-4):66-84.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700