太湖流域典型区50年代以来极值水位时空变化

doi:10.11821/yj2011060011

地理研究 ›› 2011, Vol. 30 ›› Issue (6): 1077-1088.doi: 10.11821/yj2011060011

太湖流域典型区50年代以来极值水位时空变化

尹义星^1,2, 许有鹏², 陈莹³

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;
3. 福建师范大学地理科学学院,福州 350007

收稿日期:2010-04-21 修回日期:2010-11-14 出版日期:2011-06-20 发布日期:2011-06-20
作者简介:尹义星(1974-),男,汉族,安徽和县人,博士,讲师,主要从事洪涝灾害、水文气象方面的研究。E-mail: yyxrosby@126.com
基金资助:
国家自然科学基金项目(40730635、40571025);水利部公益性行业科研专项经费项目(200701024、200901042);高校博士点基金(2006084019);江苏省自然科学基金项目(BK2006133)

Temporal and spatial changes of extreme water levels in the typical regions of Taihu Lake basin since the 1950s

YIN Yi-xing^1,2, XU You-peng², CHEN Ying³

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;
3. College of Geographic Sciences, Fujian Normal University, Fuzhou 350007, China

Received:2010-04-21 Revised:2010-11-14 Online:2011-06-20 Published:2011-06-20

摘要/Abstract

摘要： 以武澄锡虞区和阳澄淀泖区为代表,研究太湖流域典型区河网极值水位的时空变化。采用改进的MK检验和均一性检验方法检测最高和最低水位的趋势,并识别突变点;应用克里金插值技术、半变异函数方法,探讨水位变化的空间特征。研究认为:时间变化上,1950年代以来研究区各站点极值水位存在一致的上升趋势,且以最低水位上升更为显著;最高、最低水位在1980年代左右普遍性地经历一次突变。另外,历年最高水位的年际变异大于最低水位。空间变化上,突变后最高与最低水位增幅较大的站点位于阳澄淀泖区,最高与最低水位变差系数的等值线梯度均增大,即空间变异加大;半变异函数分析结果表明,突变后极值水位的空间自相关性减弱,这与流域高强度的人类活动干扰有关。分析认为,研究区河网极值水位与历年降水的变化之间存在差异,而人类活动影响在水位变化过程中发挥着越来越重要的作用。

关键词: 极值水位, 时空变化, 太湖流域典型区, 降水, 人类活动

Abstract: Taking Wuchengxiyu and Yangchengdianmao regions as examples, the paper investigates the temporal and spatial changes of extreme water levels in the river networks of Taihu Lake basin. The improved MK test and homogeneity test are used to detect trend and change points in the series of maximum and minimum water levels, and Kriging and semivariogram methods are adopted to analyze the spatial characteristics of water level changes. Furthermore, the relationship among extreme water levels, precipitation and human activities are discussed. Some meaningful results are obtained as follows. As for temporal changes, there is a global increasing trend in both the low water level (LWL) and high water level (HWL), with the increase of LWL being more significant than that of HWL. Both LWL and HWL experienced an abrupt change around the 1980s. What's more, the temporal variations of annual HWL are bigger than those of the LWL. As for spatial changes, the results of contour analysis show that the maximum increment magnitudes of HWL and LWL are observed in Yangchengdianmao Region. And the gradient of HWL and LWL variation coefficients is on the rise, indicating that their spatial variability has increased. Besides, the spatial autocorrelation of extreme water levels has been weakened after the abrupt change according to semivariogram analysis, which might be mainly due to the extensive human disturbance. The paper comes to the conclusion that there are differences between the characteristics of extreme water level changes and rainfall variations in the study region, and anthropogenic influences have played more and more important roles in the process of water level changes.

Key words: extreme water level, temporal and spatial changes, typical regions of Taihu Lake basin, precipitation, human activity

尹义星, 许有鹏, 陈莹. 太湖流域典型区50年代以来极值水位时空变化[J]. 地理研究, 2011, 30(6): 1077-1088.

YIN Yi-xing, XU You-peng, CHEN Ying. Temporal and spatial changes of extreme water levels in the typical regions of Taihu Lake basin since the 1950s[J]. GEOGRAPHICAL RESEARCH, 2011, 30(6): 1077-1088.

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太湖流域典型区50年代以来极值水位时空变化

Temporal and spatial changes of extreme water levels in the typical regions of Taihu Lake basin since the 1950s

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