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太湖流域腹部地区水位对降水变化及城镇化的响应

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  • 1. 南京信息工程大学 应用水文气象研究院,南京 210044;
    2. 南京大学 地理与海洋科学学院,南京 210093
尹义星(1974- ),男,安徽和县人,博士,主要从事流域洪涝灾害、水文气象方面的研究。 E-mail: yyxrosby@126.com

收稿日期: 2010-01-21

  修回日期: 2011-01-31

  网络出版日期: 2011-05-20

基金资助

国家自然科学基金重点项目(40730635);水利部公益性行业科研专项经费项目(200701024,200901042);国家自然科学基金项目(40571025);高校博士点基金(2006084019)。

Response of Water Levels to Precipitation Changes and Regional Urbanization in the Core Regions of the Taihu Lake Basin

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  • 1. Applied Hydrometeorological Research Institute, Nanjing University of Information Science and Technology, Nanjing 210044, China;
    2. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, China

Received date: 2010-01-21

  Revised date: 2011-01-31

  Online published: 2011-05-20

摘要

20世纪80年代以来,在气候和人类活动因素的影响下,太湖流域汛期河网水位上升明显,洪涝频发。论文基于流域腹部地区站点日降水和水位资料,对历年降水和水位进行分等级研究,分析它们的变化趋势及差异;并采用两变量弹性分析方法探讨水位对降水变化和以城镇化为代表的人类活动响应的敏感性。结果表明:①1954—2006年汛期和非汛期高等级(8~10级)降水占相应时段总降水的贡献率呈上升趋势,而低等级(1~3级)降水贡献率呈下降趋势,即降水集中程度在增加。水位变化呈现类似特点,并且高等级水位的集中程度增加更为显著。②基准期(汛期1954—1985年,非汛期1954—1987年)水位变化对城镇化的弹性系数均未达到显著性水平,而相对期(汛期1986—2006年,非汛期1988—2006年)的城镇化弹性系数比较显著,其造成水位变化的贡献率在非讯期已接近降水的贡献率。因此,以快速城镇化为代表的人类活动影响,在研究区水位变化中发挥越来越重要的作用。

本文引用格式

尹义星, 许有鹏 . 太湖流域腹部地区水位对降水变化及城镇化的响应[J]. 自然资源学报, 2011 , 26(5) : 769 -779 . DOI: 10.11849/zrzyxb.2011.05.005

Abstract

The water level of river network significantly increased and flood disasters occurred frequently in the Taihu Lake Basin at the end of the 20th century under the influence of climatic and anthropogenic factors. This paper makes a classification analysis of precipitation and water level series and explores the trends of their changes based on daily rainfall and water level data. A two-parameter elasticity analysis is adopted to investigate the sensitivity of water level to precipitation changes and urbanization which is representative of human activities. The main results are as follows: First, the contribution of low ranks (Ranks 1-3) of precipitation in flood and non-flood seasons to the total precipitation in the same period is on the decrease while the contribution of the high ranks (Ranks 8-10) is on the increase, thus the concentration of precipitation increases. The characteristics of water level are similar to those of the precipitation. However, the concentration of high rank water levels increases much more significantly than that of the rainfall. Second, the elasticity of urbanization during baseline period (1954-1985 for flood season and 1954-1987 for non-flood season) is not significant at the 5% level, while it is significant during the comparison period and the contribution of urbanization is near that of the precipitation. The paper draws a conclusion that human activities characterized by fast urbanization have played an important role in the changes of water level in the core region of the Taihu Lake Basin since the 1980s. The results of the paper may provide support for flood control and urban planning and management in the study area.

参考文献

[1] 黄俊雄, 徐宗学. 太湖流域1954—2006年气候变化及其演变趋势[J]. 长江流域资源与环境, 2009, 18(1): 33-40. [2] 陈家其. 长江三角洲城市建设发展与城市水害[J]. 长江流域资源与环境, 1995, 4(3): 202-208. [3] 王西琴, 张远, 张艳会. 渭河上游天然径流变化及其自然与人为因素影响贡献量[J]. 自然资源学报, 2006, 21(6): 981-990. [4] 叶许春, 张奇, 刘健, 等. 气候变化和人类活动对鄱阳湖流域径流变化的影响研究[J]. 冰川冻土, 2009, 31(5): 835-842. [5] Zhao Fangfang, Xu Zongxue, Zhang Lu, et al. Streamflow response to climate variability and human activities in the upper catchment of the Yellow River Basin[J]. Science in China Series E: Technological Sciences, 2009, 52(11): 1-8. [6] Chen Zhongyuan, Wang Zhanghua. Yangtze Delta, China: Taihu lake-level variation since the 1950s, response to sea-level rise and human impact [J]. Environmental Geology, 1999, 37(4): 333-339. [7] Hu Qingfang, Wang Yintang. Impact assessment of climate change and human activities on annual highest water level of Taihu Lake [J]. Water Science and Engineering, 2009, 2(1): 1-15. [8] 尹义星, 许有鹏, 陈莹. 湖流域典型区50年代以来极值水位时空变化研究[J]. 地理研究, 待刊. [9] 毛锐, 李国砚, 刘晓玫. 太湖流域汛期河湖等水位线的判读及其应用[J]. 湖泊科学, 2007, 19(4): 413-420. [10] Sheng Jingfen, John P Wils. Watershed urbanization and changing flood behavior across the Los Angeles metropolitan region [J]. Natural Hazards, 2009, 48: 41-57. [11] Hicks R W B, Woods S D. Pollutant load, population growth and land use. Progress: Water Environment Research Foundation. 2000, 11: 10. [12] 江苏省地方志编撰委员会. 江苏省志·人口志[M]. 北京: 方志出版社, 1999. [13] Osborn T J, Hulme M, Jones P D, et al. Observed trends in the daily intensity of United Kingdom precipitation [J]. International Journal of Climatology, 2000, 20: 347-364. [14] Karl T R, Knight R W. Secular trends of precipitation amount frequency and intensity in the United States [J]. Bulletin of the American Meteorological Society, 1998, 79: 231-241. [15] Sankarasubramaniam A, Vogel R M, Limburner J F. Climate elasticity of streamflow in the United States [J]. Water Resources Research, 2001, 37: 1771-1781. [16] 谢平, 陈广才, 雷红富, 等. 变化环境下地表水资源评价方法[M]. 北京: 科学出版社, 2009. [17] 杨桂山, 王德建, 等. 太湖流域经济发展·水环境·水灾害[M]. 北京: 科学出版社, 2003. [18] 李燕, 李恒鹏. 太湖流域土地利用变化的水文效应及其风险评价[J]. 水土保持学报, 2007, 27(5): 37-40.
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