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韩 非, 陈影影, 于世永, 栗文佳, 张云峰, 陈诗越.1954-2018年东平湖水位变化特征及驱动因素分析水资源与水工程学报[J].,2020,31(3):102-109
1954-2018年东平湖水位变化特征及驱动因素分析
Characteristics and driving factors of water level variations of Dongping Lake between 1954 and 2018
  
DOI:10.11705/j.issn.1672-643X.2020.03.15
中文关键词:  水位变化  趋势分析  周期特征  驱动因素  东平湖
英文关键词:water level variation  trend analysis  periodic characteristics  driving factor  Dongping Lake
基金项目:国家自然科学基金项目(41701101、41501003、41672345、41871073); 黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG1902); 江苏师范大学博士人才项目(17XLR003); 江苏省研究生科研与实践创新计划项目(KYCX20_2275); 江苏高校优势学科建设工程资助项目
作者单位
韩 非1, 陈影影1, 于世永1, 栗文佳1, 张云峰2, 陈诗越1 (1.江苏师范大学 地理测绘与城乡规划学院 江苏 徐州 221116 2.盐城师范学院 江苏沿海开发研究院 江苏 盐城 224007) 
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中文摘要:
      依据东平湖1954-2018年水位资料,采用Mann-Kendall突变检验、小波分析等方法,分析了1958-2018年东平湖的水位变化特征,探讨了其变化的自然和人为因素。研究结果表明:1958-2018年东平湖水位年际变化幅度较大,总体呈现中-低-高的变化特征;年际水位周期变化具有28a和40a的时间尺度特征。人类活动影响下的入湖径流量变化是东平湖水位变化的主要因素,气候因素也起到一定程度的作用。1958年之前,东平湖与黄河自然联通,水位变化受黄河和大汶河来水影响较大;1958年以后,东平湖与黄河水文系统被人为控制,水位变化主要受大汶河入湖径流量变化的影响;1970年以后,气候变暖加剧,降水量增加影响了水位的变化;2013年南水北调东线工程实施后,人为因素的影响进一步加大。
英文摘要:
      According to the water level records of Dongping Lake of recent 65 years (1954-2018), Mann-Kendall mutation test and Morlet analysis were used to analyze the water level variation characteristics of Dongping Lake between 1954 and 2018, and the influencing factors of nature and human activities were discussed. The results showed that the inter-annual water levels of Dongping Lake in the past 65 years changed greatly, and the overall characteristics showed a medium-low-high variation trend, with the periodic time-scale features of 28 years and 40 years. The change of inflow runoff under the influence of human activities was the main factor of water level variations in Dongping Lake, and the climatic factors played an important role too. Due to the natural connection between Dongping Lake and the Yellow River, the water level of Dongping Lake was greatly affected by the inflow from the Yellow River and the Dawen River before 1958. Since then, the hydrological system of Dongping Lake and the Yellow River was artificially controlled, so the water level of Dongping Lake was mainly affected by the inflow from Dawen River. The water level changed accordingly after 1970, due to the increase of precipitation caused by the worsening of globalwarming. In addition, the impact of the human activities further increased after the implementation of the East Route Project of South-to-North Water Transfer in 2013.
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