文章摘要
杜一衡, 郝振纯, 李伟玲, 鞠 琴, 鲁承阳, 畅俊杰.黄河源区河道冰凌特征变化及影响因素分析Journal of Water Resources and Water Engineering[J].,2014,25(5):32-36
黄河源区河道冰凌特征变化及影响因素分析
Analysis of change and influence factor of ice regime character in Yellow River source area
  
DOI:10.11705/j.issn.1672-643X.2014.05.007
中文关键词: 黄河源区; 凌情特征; 变化趋势  气温
英文关键词: Yellow River source area  character of ice regime  change trend  temperature
基金项目:全球变化研究国家重大科学研究计划项目(2010CB951103);国家自然科学基金重点项目(40830639);2011年度高等学校博士学科点专项科研基金(20110094110013);国家重点实验室团队项目(1069-50985512)
Author NameAffiliation
DU Yiheng1,HAO Zhenchun1, LI Weiling1,JU Qin1,LU Chengyang2 , CHANG Junjie2 (1.河海大学 水文水资源与水利工程科学国家重点实验室 江苏 南京 210098 2.黄河水利委员会河源研究院 甘肃 兰州 730000) 
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中文摘要:
      黄河流域是我国凌汛灾害常发的地区,其中黄河源区是黄河上游凌情研究的空白区。为掌握该区域的凌情规律,对黄河沿-唐乃亥河段黄河沿、吉迈、玛曲3个常封断面的气象资料(1960-1987,2007-2011)和水文资料(1960-1987,2007-2011)进行研究,分析3个站的封河、开河日期以及冬季最大冰厚的变化规律,得出黄河源区封河从黄河沿附近开始向下游延伸,封河日期和开河日期均有推迟趋势,但总封冻天数在减少,冬季最大冰厚则各站趋势不同。通过对冬季气温、流量等因素进行分析,得出冬季累计负气温和冬季平均流量对于凌情主要特征的影响十分显著,可以作为预报因子进行进一步的研究。
英文摘要:
      The Yellow River is one of the most seriously-affected areas where the melting ice flood disasters often take place. The source area of the Yellow River is the research gap of ice-slush..Based on analyzing the meteorological and hydrological data of the Yellow River source area, this paper selected three representative cross sections, summarized main characters of the ice regime. It then analyzed the dates of freeze-up and break-up of the river ,and the change rule of the largest ice thickness in winter.The result shows that the freeze-up goes from upstream to downstream.The dates have delaying trend,but the total number of freeze-up days is decreased and the largest ice thickness each station in winter is different. meanwhile the break-up process goes on the contrary.The main influence factors of ice regime are air temperature, average flow in winter witch can be taken as forcast factors to further research.
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