基于双累积曲线法的径流变化成因分析
The Causes of Runoff Variation Based on Double Cumulative Curve Analysis Method
DOI: 10.12677/JWRR.2012.14028, PDF, HTML,  被引量 下载: 3,695  浏览: 10,531  国家自然科学基金支持
作者: 胡彩虹*, 王艺璇, 管新建*, 石志民*:郑州大学水利与环境学院
关键词: 气候变化人类活动汾河流域径流变化Climate Change; Human Activities; Fenhe River Basin; Runoff Variation
摘要: 合理分析气候变化和人类活动对河川径流的影响,是环境变化影响研究领域中的科学问题,由于现阶段气候变化和剧烈的人类活动,致使径流形成机理和规律发生了变化。本文提出了在采用统计学方法分析径流和降水变异分析的基础上,将径流分成基准期和变化期,以基准期为基础建立降水径流双累积曲线模型,定量分析变化期气候变化和人类活动对径流的影响。以汾河流域为例进行了实例研究,研究结果表明,汾河入黄河津站实测径流减少趋势明显,1981年为径流的突变年份。1981年后气候变化和人类活动的综合作用致使实测径流减少明显。其中,人类活动致使径流深减少了13.0 mm,贡献率为84.4%,降水减少致使径流深减少了2.4 mm,贡献率为15.6%
Abstract: Reasonable analysis on influences of climate change and human activities on runoff is a scientific question of environmental changes. Runoff generation mechanism and rules has changed due to the climate change and intense human activities. Double Mass Curve method was built based on the baseline period to quantify the influence of climate change and human activities on runoff according to the statistics results. The Fenhe river basin was chosen as case study. The results show that the runoff of the Fenhe river basin had a decreasing trend, and the mutation year is 1981. The reasons of observed runoff reducing caused by combined effect of climate change and human activities after 1981. The affect amounts of runoff are 15.4 mm, in which 13.0 mm is caused by the human activities and 2.4 mm is caused by climate change, the contribution rate are 84.4% and 15.6%, respectively.
文章引用:胡彩虹, 王艺璇, 管新建, 石志民. 基于双累积曲线法的径流变化成因分析[J]. 水资源研究, 2012, 1(4): 204-210. http://dx.doi.org/10.12677/JWRR.2012.14028

参考文献

[1] LIU, Q., YANG, Z. F., CUI, B. S., et al. Spatial and temporal variability of annual precipitation during 1961-2006 in Yellow River Basin, China. Journal of Hydrology, 2008, 361: 330-338.
[2] 樊辉, 杨晓阳. 黄河干支流径流量与输沙量年际变化特征 [J]. 泥沙研究, 2010, 4: 11-15. PAN Hui, YANG Xiaoyang. The inter-annual features of runoff and sediment yield in Yellow River. Chinese Journal of Sediment Research, 2010, 4: 11-15. (in Chinese)
[3] 粟晓玲, 康绍忠, 魏晓妹. 气候变化和人类活动对渭河流域入黄径流的影响[J]. 西北农林科技大学学报(自然科学版), 2007, 35(2): 153-159. LI Xiaoling, KANG Shaozhong and WEI Xiaomei. Impact of climate change and human activity on the runoff of Wei River basin to the Yellow River. Journal of Northwest Forestry Science and Technology University (Natural Science Edition), 2007, 35(2): 153-159. (in Chinese)
[4] 张淑兰, 王彦辉, 于澎涛, 等. 定量区分人类活动和降水量变化对泾河上游径流变化的影响[J]. 水土保持学报, 2010, 24(4): 53-58. ZHANG Shulan, WANG Yanhui, YU Pengtao, et al. Study for separating the impact of precipitation variation and human activ-ities on runoff change of the upper reaches of Jing River. Chinese Journal of Soil and Water Conservation, 2010, 24(4): 53-58. (in Chinese)
[5] MIAO, C. Y., NI, J. R., BORTHWICK, A. G. L., et al. A preliminary estimate of human and natural contributions to the changes in water discharge and sediment load in the Yellow River. Global and Planetary Change, 2011, 76: 196-205.
[6] 贾仰文, 高辉, 牛存稳, 等. 气候变化对黄河源区径流过程的影响[J]. 水利学报, 2008, 39(1): 52-58. JIA Yangwen, GAO Hui, NV Cunwen, et al. Impact of climate change on runoff process in headwater area of the Yellow River. Chinese Journal of Hydraulic Engineering, 2008, 39(1): 52-58. (in Chinese)
[7] 陈忠升, 陈亚宁, 徐长春. 近50a来塔里木河干流年径流量变化趋势及预测[J]. 干旱区地理, 2011, 31(1): 43-51. CHENG Zhongsheng, CHENG Yaning and XU Changchun. Change trend and prediction of annual runoff in mainstream area of the Tarim River in recent 50 years. Chinese Journal of Arid Land Geography, 2011, 31(1): 43-51. (in Chinese)
[8] 穆兴民, 张秀勤, 高鹏, 等. 双累积曲线方法理论及在水文气象领域应用中应注意的问题[J]. 水文, 2010, 30(4): 47-51. MU Xingming, ZHANG Xiuqing, GAO Peng, et al. Theory of double mass curves and its applications in hydrology and meteorology. Chinese Journal of Hydrological, 2010, 30(4): 47-51. (in Chinese)
[9] 胡彩虹, 管新建, 吴泽宁, 等. 水土保持措施和气候变化对汾河水库入库径流贡献定量分析[J]. 水土保持措施, 2011, 25(5): 12-16. HU Caihong, GUAN Xinjian, WU Zening, et al. Analysis for contribution of soil and water conservation and climate change to runoff in the upper reaches of Fenhe reservation. Chinese Journal of Soil and Water Conservation, 2011, 25(5): 12-16. (in Chi-nese)
[10] 赵云, 胡彩虹, 胡珊. 汾河和沁河流域入黄径流锐减事实分析[J]. 水电能源科学, 2012, 30(3): 31-34. ZHAO Yun, HU Caihong and HU Sanshan. Facts analysis of significant reduction in runoff of Fenhe and Qinhe Basin. Chi- nese Journal of Water Resources and Power, 2012, 30(3): 31-34. (in Chinese)
[11] 刘宇峰, 孙虎, 原志华. 近60年来汾河入黄河水沙演变特征及驱动因素[J]. 山地学报, 2010, 28(6): 668-673. LIU Yufeng, SUN Hu and YUAN Zhihua. Characteristics and driving factors of runoff and sediment changes flux into the Yel- low River from Fenhe River in recent 60 years. Chinese Journal of Journal of Mountain Science, 2010, 28(6): 668-673. (in Chi- nese)
[12] 赵学敏, 胡彩虹, 张丽娟, 等. 汾河流域降水变化趋势的气候分析[J]. 干旱区地理, 2007, 30(1): 52-59. ZHAO Xuemin, HU Caihong, ZHANG Lijuan, et al. Climatic analysis of precipitation change trend over the Fenhe River Basin. Arid Land Geography, 2007, 30(1): 52-59. (in Chinese)
[13] 赵学敏, 胡彩虹, 吴泽宁, 等. 汾河流域降水及旱涝时空结构特征[J]. 干旱区研究, 2007, 24(3): 349-354. ZHAO Xuemin, HU Caihong, WU Zening, et al. Analysis on the spatiotemporal change of precipitation, flood and drought in the Fenhe River Basin. Arid Zone Research, 2007, 24(3): 349-354. (in Chinese)
[14] 郝福华. 汾河水库流域水土保持治理减沙与径流变化分析[J]. 水利水电技术, 2009, 40(5): 61-63. HAO Fuhua. Analysis on run-off variation and sediment reduce- tion for water and soil conservation of Fenhe River Basin. Chi- nese Journal of Water Resources and Hydropower Engineering, 2009, 40(5): 61-63. (in Chinese)