气候变化和人类活动对白洋淀上游水源区径流的影响

doi:10.11821/xb201201007

地理学报 ›› 2012, Vol. 67 ›› Issue (1): 62-70.doi: 10.11821/xb201201007

气候变化和人类活动对白洋淀上游水源区径流的影响

胡珊珊^1,2, 郑红星¹, 刘昌明^1,3, 于静洁¹, 王中根¹

1. 陆地水循环及地表过程重点实验室, 中国科学院地理科学与资源研究所, 北京 100101;
2. 中国科学院研究生院, 北京 100049;
3. 北京师范大学水科学研究院, 北京 100875

收稿日期:2011-07-29 修回日期:2011-10-18 出版日期:2012-01-20 发布日期:2012-01-20
通讯作者: 郑红星, 男, 副研究员, 中国地理学会会员(S110001621M), 主要从事水文水资源研究。E-mail: zhenghx@igsnrr.ac.cn
基金资助:
国家自然科学基金项目(40830636; 40971023)

Assessing the Impacts of Climate Variability and Human Activities on Streamflow in the Water Source Area of Baiyangdian Lake

HU Shanshan^1,2, ZHENG Hongxing¹, LIU Changming^1,3, YU Jingjie¹, WANG Zhonggen¹

1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China;
3. College of Water Sciences, Beijing Normal University, Beijing 100875, China

Received:2011-07-29 Revised:2011-10-18 Online:2012-01-20 Published:2012-01-20
Supported by:
National Natural Science Foundation of China, No.40830636; No.40971023

摘要/Abstract

摘要： 白洋淀是华北平原最大的湖泊湿地,对维持华北平原生态平衡具有极其重要的作用。近年来,白洋淀流域水源减少已经引起了严重的生态环境问题,本文以唐河上游流域为例,根据流域内1960-2008 年水文气象数据,采用气候弹性系数和水文模拟方法,研究了气候变化和人类活动对白洋淀上游水源区径流量的影响。结果表明：年径流下降趋势显著,下降速率为1.7 mm/a,且径流在1980 年前后发生了突变;气候变化对唐河上游流域径流减少的贡献率为38%~40%,人类活动对径流的减少起主导作用,为60%~62%。为维持白洋淀的生态功能,必须保证一定的最小生态需水量,开展湿地生态用水调度与监管。

关键词: 唐河, 气候变化, 人类活动, 弹性系数, 水文模型, 白洋淀流域

Abstract: As the largest wetland in the North China Plain, Baiyangdian Lake plays an important role in maintaining water balance and ecological health of NCP. In the past few decades, the decreasing streamflow in Baiyangdian Basin associated with climate variability and human activities has caused a series of water and eco-environmental problems. In this study, we quantified the impacts of climate variability and human activities on streamflow in the water source area of Baiyangdian Lake, based on analyses of hydrologic changes of upper Tanghe catchment from 1960 to 2008. Climate elasticity method and hydrological modeling method were used to distinguish the effects of climate variability and human activities. The results showed that the annual streamflow decreased significantly (P > 0.05) by 1.7 mm/a and an abrupt change was identified around the year 1980. The quantification results indicated that climate variations accounted for 38%-40% of decrease in streamflow, while human activities accounted for 60%-62%. Therefore, human activities played a dominant influence in the decline of the streamflow in the water source area of Baiyangdian Lake. To keep the ecosystem health of Baiyangdian Lake, we suggest that minimum eco-water demand and integrated watershed management should be guaranteed in the future.

Key words: climate variability, human activities, climate elasticity, hydrological model, Baiyangdian Lake, Tanghe River

胡珊珊, 郑红星, 刘昌明, 于静洁, 王中根. 气候变化和人类活动对白洋淀上游水源区径流的影响[J]. 地理学报, 2012, 67(1): 62-70.

HU Shanshan, ZHENG Hongxing, LIU Changming, YU Jingjie, WANG Zhonggen. Assessing the Impacts of Climate Variability and Human Activities on Streamflow in the Water Source Area of Baiyangdian Lake[J]. Acta Geographica Sinica, 2012, 67(1): 62-70.

参考文献

[1] Gao Yanchun, Wang Han, Long Di. Changes in hydrological conditions and the eco-environmental problems inBaiyangdian watershed. Resources Science, 2009, 31(9): 1506-1513. [高彦春, 王晗, 龙笛. 白洋淀流域水文条件变化和面临的生态环境问题. 资源科学, 2009, 31(9): 1506-1513.]
[2] Liu Keyan, Zhang Lu, Zhang Guanghui et al. The impact of human activities on runoff in Baiyangdian basin in NorthChina. Journal of China Hydrology, 2007, 27(6): 6-10. [刘克岩, 张橹, 张光辉等. 人类活动对华北白洋淀流域径流影响的识别研究. 水文, 2007, 27(6): 6-10.]
[3] Li Yinghua, Cui Baoshan, Yang Zhifeng. Influence of hydrological characteristic change of Baiyangdian on theecological environment in wetland. Journal of Natural Resources,, 2004, 19(1): 62-68. [李英华, 崔保山, 杨志峰. 白洋淀水文特征变化对湿地生态环境的影响. 自然资源学报, 2004, 19(1): 62-68.]
[4] Gong Ran. Water change in Baiyangdian Lake and affecting factors. Geography and Territorial Research, 1993, 9(2):36-40. [弓冉. 白洋淀水量变化原因分析. 地理学与国土研究, 1993, 9(2): 36-40.]
[5] Bai Debin, Ning Zhenping. An elementary analysis to Baiyangdian dried-up. China Flood & Drought Management,2007, (2): 46-48. [白德斌, 宁振平. 白洋淀干淀原因浅析. 中国防汛抗旱, 2007, (2): 46-48.]
[6] Montenegro A, Ragab R. Hydrological response of a Brazilian semi-arid catchment to different land use and climatechange scenarios: A modelling study. Hydrological Processes, 2010, 24(19): 2705-2723.
[7] Wang Gangsheng, Xia Jun, Chen Ji. Quantification of effects of climate variations and human activities on runoff by amonthly water balance model: A case study of the Chaobai River basin in northern China. Water Resources Research,2009, 45(7), W00A11, doi: 10.1029/2007WR006768.
[8] Li Daofeng, Tian Ying, Liu Changming. Distributed hydrological simulation of the source regions of the Yellow Riverunder environmental changes. Acta Geographica Sinica, 2004, 59(4): 565-573. [李道峰, 田英, 刘昌明. 黄河河源区变化环境下分布式水文模拟. 地理学报, 2004, 59(4): 565-573.]
[9] Leavesley George H. Modeling the effects of climate change on water resources: A review. Climatic Change, 1994, 28(1): 159-177.
[10] Legesse Dagnachew, Vallet Coulomb Christine, Gasse Francoise. Hydrological response of a catchment to climate andland use changes in Tropical Africa: Case study South Central Ethiopia. Journal of Hydrology, 2003, 275(1/2): 67-85.
[11] Fu Guobin, Charles Stephen P, Chiew Francis H S. A two-parameter climate elasticity of streamflow index to assessclimate change effects on annual streamflow. Water Resources Research, 2007, 43(11), W11419, doi: 10.1029/2007WR005890.
[12] Sankarasubramanian A, Vogel R M, Limbrunner J F. Climate elasticity of streamflow in the United States. WaterResources Research, 2001, 37(6): 1771-1781.
[13] Allen R G, Pereira L S, Raes D et al. Crop evapotranspiration: Guidelines for computing crop water requirements.FAO Irrigation and Drainage Paper 56. FAO, Rome, 1998: 300.
[14] Mann H B. Nonparametric tests against trend. Econometrica: Journal of the Econometric Society, 1945, 13(3): 245-259.
[15] Kendall M G. Rank Correlation Measures. London: Charles Griffin, 1975.
[16] Buishand T A. Some methods for testing the homogeneity of rainfall records. Journal of Hydrology, 1982, 58(1/2):11-27.
[17] Chen J, Gupta A K. Parametric statistical change point analysis. Birkh User, 2000.
[18] Lane Patrick N, Lane J, Best Alice E et al. The response of flow duration curves to afforestation. Journal ofHydrology, 2005, 310(1-4): 253-265.
[19] Mu Xingming, Gao Peng, Ba Sangchilie et al. Estimating the impact of conservation measures on stream-flow regimein catchments of the Loess Plateau, China. Advances in Earth Science, 2008, 23(4): 382-389. [穆兴民, 高鹏, 巴桑赤烈等. 应用流量历时曲线分析黄土高原水利水保措施对河川径流的影响. 地球科学进展, 2008, 23(4): 382-389.]
[20] Schaake J C. From climate to flow. Climate Change and US Water Resources, 1990: 177-206.
[21] Budyko M I. Evaporation under Natural Conditions. Leningrad: Gidrometeoizdat, 1948.
[22] Arora V K. The use of the aridity index to assess climate change effect on annual runoff. Journal of Hydrology, 2002,265(1-4): 164-177.
[23] Dooge J C I, Bruen M, Parmentier B. A simple model for estimating the sensitivity of runoff to long-term changes inprecipitation without a change in vegetation. Advances in Water Resources, 1999, 23(2): 153-163.
[24] Ol'dekop E M. On evaporation from the surface of river basins (in Russian). Transactions on MeteorologicalObservations, 1911.
[25] Fu Baopu. On the calculation of the evaporation from land surface. Scientia Atmospherica Sinica, 1981, 5(1): 23-31.[傅抱璞. 论陆面蒸发的计算. 大气科学, 1981, 5(1): 23-31.]
[26] Zhang L, Dawes W R, Walker G R. Response of mean annual evapotranspiration to vegetation changes at catchmentscale. Water Resources Research, 2001, 37(3): 701-708.
[27] Liu Changming, Wang Zhonggen, Zheng Hongxing et al. Development of hydro-informatic modelling system and itsapplication. Science in China Series E: Technological Sciences, 2008, 51(4): 456-466. [刘昌明, 王中根, 郑红星等.HIMS系统及其定制模型的开发与应用. 中国科学: E辑, 2008, 51(3): 350-360.]
[28] Liu C M, Wang G T. The estimation of small-watershed peak flows in China. Water Resources Research, 1980, 16(5):881-886.
[29] Yang Yonghui, Tian Fei. Abrupt change of runoff and its major driving factors in Haihe River Catchment, China.Journal of Hydrology, 2009, 374(3/4): 373-383.
[30] Hu Shanshan, Zhao Fan, Zhang Guangying. Change of rainfall-runoff and its causes in the upper Tang Watershed inrecent 40 years. South-to-North Water Transfers and Water Science & Technology, 2009, 7(5): 73-75. [胡珊珊, 赵帆,张广英. 近40 年来唐河上游降水-径流变化及原因探讨. 南水北调与水利科技, 2009, 7(5): 73-75.]
[31] Cheng Jianjing. The existed problems & counter measures on utilization of water conservancy & hydropower of theTanghe river valley. Groundwater, 2003, 25(1): 49-51. [程建京. 唐河流域水利水电资源开发利用存在的问题及对策.地下水, 2003, 25(1): 49-51.]

气候变化和人类活动对白洋淀上游水源区径流的影响

Assessing the Impacts of Climate Variability and Human Activities on Streamflow in the Water Source Area of Baiyangdian Lake

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