| 1766～1911年黄河中游汛期建立时间研究 |
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| 引用本文： | 潘威,刘楠,庄宏忠.1766～1911年黄河中游汛期建立时间研究[J].干旱区资源与环境,2012(5):41-45. |
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| 作者姓名： | 潘威 刘楠 庄宏忠 |
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| 作者单位： | 陕西师范大学西北历史环境与经济社会发展研究院GIS实验室;中国科学院地理科学与资源研究所;南京信息工程大学语言文化学院 |
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| 基金项目： | 国家重点基础研究发展规划(973计划)项目(2010CB950100);复旦大学整体推进人文社会科学(985计划)项目(2011RWXKZD022);陕西师范大学人文社会科学基金项目(09SYB06)资助 |
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| 摘 要： | 利用清代奏报中保留的汛期涨水尺寸记录,近现代以来黄河中游水文站存在的水位信息器测数据,基于1766～1911年黄河中游万锦滩(位于今河南省三门峡市)水位志桩所载涨水时间,在"侯"尺度下建立了研究时段内三门峡断面的汛期开始时间。结果表明:1766～1911年,1840年代前中游汛期开始时间在平均水平;1840～1860年代汛期建立时间偏晚;1860～1890年代再次开始提前。在研究时段内黄河中游汛期开始时间平均为7月上旬,与同时期长江中下游梅雨结束时间有很好的对应关系,但年际差异较大,夏季风雨带推移成为导致中游汛期开始时间产生波动的主要驱动因素。
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| 关 键 词： | 水位志桩 黄河中游 汛期 夏季风雨带 |
Study on the beginning time of flood season in the middle reaches of Yellow River,1766-1911 |
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| PAN Wei,LIU Nan,ZHUANG Hongzhong.Study on the beginning time of flood season in the middle reaches of Yellow River,1766-1911[J].Journal of Arid Land Resources and Environment,2012(5):41-45. |
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| Authors: | PAN Wei LIU Nan ZHUANG Hongzhong |
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| Institution: | 1(1.Center for Historical Environment and Socio-economic Development in Northwest,China Institute of Geographic Sciences and Natural Resources Research,Shaanxi Normal University,Xi’an 710062,P.R.China; 2.Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,P.R.China; 3.The Department of Chinese Language and Literature,Nanjing University of Information Science and Technology,Nanjing,Jiangsu 210044,P.R.China) |
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| Abstract: | In this study,we used the water level records of flood season for the middle reaches of the Yellow River Wanjintan in the Sanmenxia city,Henan province by Qing government and modern hydrological stations during 1766 ~ 1911,and reconstucted the curve of floodseason beginning time under pendate scale.The results showed that before the 1840s flood season starting time was on average;in 1840s~ 1860s the flood season time was later than avwerage;in 1860 ~ 1890s,flood season time began again ahead of average.In the study period the flood season start time was at an average of in early July,with the same period with in the end time of plum rain over middle and lower Yangtze River.There is a good corresponding relationship between of them.Summer rainband in the east-middle China is the cause of flood season start time due to the fluctuation of the main driving factors. |
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| Keywords: | water level the middle reach of Yellow River flood season summer monsoon rainband |
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