气候变化影响下水资源脆弱性评估方法及其应用

doi:10.11867/j.issn.1001-8166.2012.04.0443

地球科学进展 ›› 2012, Vol. 27 ›› Issue (4): 443 -451. doi: 10.11867/j.issn.1001-8166.2012.04.0443

夏军 ^1,3，邱冰 ^1,2*，潘兴瑶 ¹，翁建武 ¹，傅国斌 ¹，欧阳如林 ¹

1.中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室，北京100101；2.中国科学院研究生院，北京100049；3.武汉大学水资源与水电工程科学国家重点实验室，湖北武汉430072

收稿日期:2011-11-14 修回日期:2012-02-17 出版日期:2012-04-10
通讯作者: 邱冰（1983-），女，山东高密人，博士研究生，主要从事气候变化对水资源影响研究. E-mail:qiubong07@mails.gucas.ac.cn
基金资助:
国家重点基础研究发展计划项目“气候变化对中国东部季风区陆地水循环与水资源安全的影响及适应对策”（编号：2010CB428406）；中国科学院对外合作重点项目计划“中荷JSTP‘黄河与莱茵河三角洲海水入侵的检测与模拟研究’”（编号：GJHZ1016）资助.

Assessment of Water Resources Vulnerability under Climate Change and Human Activities

Xia Jun ^1,3，Qiu Bing ^1,2，Pan Xingyao ¹，Weng Jianwu ¹，Fu Guobin ¹，Ouyang Rulin ¹

1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing100101, China;
2. Graduate University of Chinese Academy of Sciences, Beijing100049, China;
3.State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan430072, China

Received:2011-11-14 Revised:2012-02-17 Online:2012-04-10 Published:2012-04-10

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气候变化和人类活动影响下的水资源脆弱性评价，是将气候变化影响纳入水资源规划管理、提出缓解气候变化不利影响的适应性对策的重要科学依据。针对与气候变化影响的水资源系统的敏感性和抗压性相联系的脆弱性与适应性问题，提出变化环境下水资源脆弱性评估理论体系和一般性公式。进一步，以水资源供需安全为出发点，采用温度、降雨双参数弹性系数和有水资源基础，直观、简单的水资源关键性指标体系方法，提出气候变化和人类活动背景下水资源脆弱性评估模型。将模型应用于缺水最严重的海河流域，评价了现状和未来情境下流域水资源的脆弱性情况。结果表明：整体上海河流域水资源脆弱性偏高，且平原区较山区更脆弱；气候因素对流域水资源的脆弱性影响明显，未来如不采取措施，海河流域的水资源脆弱性将进一步加重。

关键词: 气候变化, 水资源脆弱性, 评估模型, 海河流域

Assessment of water resource vulnerability for identifying where water resources are potentially more vulnerable to adverse effects is a pre-requisite to take adaptation strategies. This study proposed a method for water vulnerability evaluation as a function of sensitivity to climate change, people per flow unit of one million cubic meters per year, water use to availability ratio, and per capital water use. Take the Hai River basin, the most water scarcity region in China, as an example. The vulnerability of water resources under current situation and 3 different scenarios in 2050 are evaluated. Results indicate that the plain area suffer from more serious vulnerability than mountain area; although the Hai River basin is predicted to become more moisture, vulnerability of water resources may get no improvement in the future because of the increase of water withdrawal as population and economy continue to grow.

Key words: Water resources vulnerability, Assessment method, The Hai River basin, Climate change

中图分类号:

P467

[1]John W, John K, Masahiro M, et al. Core and Periphery: A Comprehensive Approach to Middle Eastern Water[M]. London：Oxford University Press, 1997.
[2]Martin S. The Politics of Water in the Middle East: An Israeli Perspective on the Hydro-Political Aspects of the Conflict[M]. New York: St. Martin’s Press,1999:192.
[3]Philip M. Water and the New States of Central Asia[M].London: Royal Institute of International Affairs, 1997.
[4]McCarthy J J, Canziani O F, Leary N A, et al. Impacts, adaptation, and vulnerability[C]∥IPCC Climate Change 2001. Cambridge:Cambridge University Press, 2001.
[5]Qian Zhengying, Zhang Guangdou. Strategic Research on Sustainable Development of Water Resource in China[M]. Beijing: China Water & Power Press, 2001.[钱正英,张光斗. 中国可持续发展水资源战略研究[M].北京：水利水电出版社,2001.] 
[6]Qin Dahe, Ding Yihui, Su Jilan, et al. Climate and Environment Change in China(Vol.Ⅰ)—Climate and Environment Evolution[M]. Beijing: Science Press, 2005: 157-174.[秦大河,丁一汇,苏纪兰,等. 中国气候与环境演变(上卷)——气候与环境的演变及预测[M]. 北京: 科学出版社, 2005: 157-174.]
[7]Taskforce on China′s National Assessment Report on Climate Change. China′s National Assessment Report on Climate Change[M]. Beijing: Science Press, 2007.[《气候变化国家评估报告》编写委员会. 中国气候变化国家评估报告[M]. 北京: 科学出版社, 2007.]
[8]Zhai Jianqing, Zeng Xiaofan, Jiang Tong. Evolution of drought and flood pattern and its effect on water resources in China from 1961 to 2050[J]. Tropical Geography, 2011, 31(3): 237-242.[翟建青,曾小凡,姜彤.中国旱涝格局演变(1961—2050年)及其对水资源的影响[J].热带地理,2011, 31(3)：237-242.]
[9]Doerfliger N, Jeannin P Y, Zwahlen F. Water vulnerability assessment in karst environments a new method of defining protection areas using a multi-attribute approach and GIS tools[J].Environmental Geology, 1999, 39(2):165-176.
[10]Brouwer F, Falkenmark M. Climate-induced water availability changes in Europe [J]. Environmental Monitoring and Assessment, 1989, 13(1):75-98.
[11]IPCC. Climate change 1995: The science of climate change[C]∥Houghton J T, Meira Filho L G, Callander B A, et al, eds.Contribution of the Scientific Assessment Working Group (WGI) to the Second Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 1996:572.
[12]Charles J V, Pamela Green, Joseph Salisbury, et al. Global water resources: Vulnerability from climate change and population growth [J].Science,2000, 289(5 477): 284-288.
[13]Hamouda M A, Nour El-Din M M, Moursy F I. Vulnerability assessment of water resources systems in the Eastern Nile Basin [J]. Water Resources Management, 2009, 23(13): 2 697-2 725.
[14]Sullivan C A. Quantifying water vulnerability: A multi-dimensional approach [J]. Stoch Environment Research and Risk Assessment, 2010, 25(4):627-640.
[15]Liu Lüliu. Concept and qquantitive assessment of vulnerability of water resource[J]. Bulletin of Soil and Water Conservation, 2002, 22(2): 41-44.[刘绿柳．水资源脆弱性及其定量评价[J]．水土保持通报,2002,22(2)：41-44.]
[16]Tang Guoping, Li Xiubin, Liu Yanhua. Assessment method of vulnerability of water resources under global climate change [J]. Advances in Earth Science,2000, 15(3): 313-317.[唐国平,李秀彬,刘燕华．全球气候变化下水资源脆弱性及其评估方法[J]．地球科学进展,2000,15(3)：313-317.]
[17]Wang Guoqing, Zhang Jianyun, Zhang Silong. Impacts of climate change on water resources and its vulnerability in China [J]. Journal of Water Resources & Water Engineering, 2005, 16(2): 7-15.[王国庆,张建云,章四龙．全球气候变化对中国淡水资源及其脆弱性影响研究综述[J]．水资源与水工程学报,2005,16(2)：7-15.]
[18]Dong Sifang, Dong Zengchuan, Chen Kangning. Analysis of water resources system vulnerability based on DPSIR conceptual model [J]. Water Resources Projection, 2010, 26(4): 1-25.[董四方,董增川,陈康宁.基于DPSIR 概念模型的水资源系统脆弱性分析[J]. 水资源保护,2010,26（4）：1-25.]
[19]Schaake J C. From Climate to Flow[M]∥Waggoner P E ed. Climatic Change and U.S. Water Resources. John Wiley & Sons Press, 1990.
[20]Sankarasubramanian A, Richard M V. Climate elasticity of streamflow in the United States [J]. Water Resources Research, 2001, 37(6): 1 771-1 781.[21]Yu Jingjie, Fu Guobin, Cai Wenju, et al. Impacts of precipitation and temperature changes on annual streamflow in the Murray-Darling Basin [J]. Water International, 2010, 35(3): 313-323.
[22]Malin Falkenmark, David Molden. Wake up to realities of river basin closure [J]. Water Resources Development, 2008, 24(2): 201-216.
[23]Liu Chunzhen, Ying Aiwen, Yan Kai. Study of sensitivity and vulnerability of water resources to climate change in China[M]∥Fu Congbin, Yan Zhongwei, eds. Global Change and the Future Trend of Ecological Environment Evolution in China. Beijing: China Meteorological Press, 1996.[刘春蓁,英爱文,颜开.中国水资源对气候变化的敏感性及脆弱性研究[M]∥符淙斌,严中伟主编.全球变化与我国未来的生存环境.北京：气象出版社,1996.]
[24]Liu Jiufu, Guo Fang. An assessment model of climate abnormality impact on water resources in Hai River basin[J]. Advances in Water Sciences, 2011,(Suppl.):27-35.[刘九夫,郭方.气候异常对海河流域水资源评估模型研究[J].水科学进展,2011,（增刊）：27-35.]
[25]Shen Y J, Oki T, Kanae S. Future change of world water resources under SRES climate warming scenarios: A multi-model analysis[J]. IAHS Public,2007, 315: 62-70.
[26]Zhang Jianyun, Wang Guoqing. The Impact of Climate Change on Water Resources[M]. Beijing: Science Press, 2007.[张建云,王国庆.气候变化对水文水资源影响研究[M].北京：科学出版社,2007.]

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