基于DEM的清水河分布式水文模型

doi:10.13826/j.cnki.cn65-1103/x.2007.03.010

干旱区地理 ›› 2007, Vol. 30 ›› Issue (3): 364-369.doi: 10.13826/j.cnki.cn65-1103/x.2007.03.010

基于DEM的清水河分布式水文模型

丁辉^1,2, 陈亚宁¹, 李卫红¹, 陈亚鹏^1,2

1 中国科学院新疆生态与地理研究所，新疆乌鲁木齐 830011;
2 中国科学院研究生院，北京 100049

收稿日期:2006-10-18 修回日期:2007-01-09 出版日期:2007-03-25 发布日期:2026-01-23
作者简介:丁辉(1977-),男,新疆石河子人,硕士研究生,主要从事水文水资源研究.E-mail:dhnotebook@163.com
基金资助:
中国科学院知识创新工程重要方向项目(kzcx2-yw-127); 国家自然科学基金(40671014,90502004)共同资助

Distributed hydrological model based on DEM in Qingshui River Basin

DING Hu^1,2, CHEN Ya ning¹, LI Wei-hong¹, CHEN Ya peng^1,2

1 Xinjiang Institute of Ecology and Geography Chinese Academy of Science U num qi 830011, Xinjiang China;
2 Graduate University of Chinese Academy of Science Beijing 100049, China

Received:2006-10-18 Revised:2007-01-09 Published:2007-03-25 Online:2026-01-23

摘要/Abstract

摘要： 对于以冰雪融水和雨水混合补给为主的西北山区流域,需要结合山区特点建立分布式水文模型。通过取塔里木河流域中的清水河水系为研究区域,采用300 m×300 m DEM数据进行流域河网水系提取,同时用DEM数据对参数进行分布式异化,建立冰雪融水与降雨相结合的分布式水文模型。分析模拟结果表明:夏季模拟径流主峰值与实测径流值较为接近,而冬春季节两者之间的差别较大,反映了西北山区流域冰雪融水和雨水混合补给为主的特点;进而开拓塔里木河区域应用该类模型的可行性。

关键词: 分布式水文模型, DEM, 融雪, 混合补给, 清水河流域

Abstract: Hydrological model is always one of the important means for deeply probing into the laws of water cycle and water resources evolvement. Nowadays the techniques of hydrological model trend to be integrated with GIS in order to utilize the functions of GIS data management space analysis and visualization; however the DEM is the basic data of GIS With the distributed hydrological model based on DEM becoming the hotspot in hydrology, it is necessary to develop some kinds of distributed hydrological model adapting to the character of northwest mountains where snowmelt water and precipitation are the main replenishment of runoff The papers on distributed hydrological model in Tarim basin, the biggest inland river in China are seldom seen In this paper the author selects the water system of Qingshui River in the Tarim basin as the study area adopts mechanism of mixed runoff-yield constructs runoff-producing model by the grid cell then sets the parameters for basin flow concentration based on the path of runoff and adopts isochrones to develop the distributed hydrological model combining snowmelt with precipitation after distributing parameters based on the data of $300\mathrm{m}\times 300\mathrm{m}$ taking effect of hysteresis into account. The results show that the simulated peak value is similar to that of observed in summer however they are different in spring and winter which indicates the character of northwest mountains that have the main replenishment of snowmelt and precipitation for runoff again. Therefore we can confirm that the model is feasible to the Tarim River basin of to some degree

Key words: distributed hydrological mode, DEM, snowmelt mixed replenishment, Qingshui River, Basin

中图分类号:

P334

丁辉, 陈亚宁, 李卫红, 陈亚鹏. 基于DEM的清水河分布式水文模型[J]. 干旱区地理, 2007, 30(3): 364-369.

DING Hu, CHEN Ya ning, LI Wei-hong, CHEN Ya peng. Distributed hydrological model based on DEM in Qingshui River Basin[J]. Arid Land Geography, 2007, 30(3): 364-369.

参考文献

[1] Huang Ping Zhao Jiguo Research of catchment distributed digital model and its application prospects [J]. Hydrology, 1977, (5): 5-10. [黄平, 赵吉国. 流域分布型水文数学模型的研究及应用前景展望 [J]. 水文, 1997, (5): 5-10.]
[2] Wang Zhonggeng Liu Changming Wu Xianfeng A review of research on distributed hydrological model based on DEM[J]. Journal of Natural Resources 2003, 18(2): 168-171. [王中根，刘昌明，吴险峰．基于DEM的分布式水文模型研究综述[J].自然资源学报，2003, 18(2): 168-171.]
[3] Mao Weiyi, Jiang Yuanan, Li jiang—feng. Analysis on the line—ar tendency of precipitation in north Xinjiang [J]. Arid Land Geography, 2006, 29(6): 798-801. [毛炜峰, 江远安, 李江风. 新疆北部的降水量线性变化趋势特征分析 [J]. 干旱区地理, 2006, 29(6): 798-801.]
[4] Tao Hui, Song Yudong, Xu Hailiang. Variation characteristics of mountainous runoff in the Kaidu river basin. Tianshan mountains [J]. Arid Land Geography, 2007, 30(1): 44-48. [陶辉, 宋郁东, 徐海亮. 开都河天山出山径流量年际变化特征与洪水频率分析 [J]. 干旱区地理, 2007, 30(1): 44-48.]
[5] Regaard J. Terminology modeling protocol and classification of hydrological model codes [A]. In: Abbott M., Refsgaard J. Distributed hydrological modeling [C]. Kluwer Academic Publishers 1996, 28-37.
[6] Abbott M B, Bathurst J C. An introduction to the European hydrological system - System Hydrologique Europeen. SHE, 2: Structure of a physically-based distributed modeling system [D]. Journal of Hydrology, 1986, 87: 61-77.
[7] Bathhurst J C, Wicks JM, O'Connell P E. The SHE /SHESED basin scale water flow and sediment transport modeling system [A]. In: Singe V. Computer models of watershed hydrology [C]. Littleton: Water Resources Publications 1995.
[8] Calver A, Wood W L. The institute of hydrology distributed model [A]. In: Singe V P. Computer models of watershed hydrology [C]. Littleton: Water Resources Publications 1995
[9] Tribe A. Automated recognition of valley lines and drainage networks from grid digital elevation models: a review and a new method. Journal of Hydrology, 1992, 139(1): 263-293
[10] Wang Zhonggeng Liu Changming Methods of constructing distributed hydrological model based on DEM[J]. Progress in Geography, 2002, 21(5): 430-439. [王中根, 刘昌明. 基于 DEM 的分布式水文模型构建方法[J]. 地理科学进展, 2002, 21(5): 430-439.]
[11] Wang Guoqing Zhang Jianzhong Ma Jirang A snow melt nn-off model and its application on Tangnaihe Station of Huang River [J]. Northwest Water Resources & Water Engineering 1977, 2(8): 61. [王国庆, 张建中, 马吉让. 融雪径流模型及其在黄河唐乃亥站的应用 [J]. 西北水资源与水工程, 1997, 2(8): 61.]
[12] Zhao Renjun Hydrological simulation of watershed-X in' anjiang Model & Shanbeimode[M]. Beijing Water Conservancy & Elec-tric Power Press 1984. [赵人俊. 流域水文模拟——新安江模型与陕北模型[M]. 北京：水利电力出版社，1984.]
[13] Zhang Xiaoyong Liu Gengnian A review of the hydrological model in the glacierized drainage basin [J]. Research of Soil and Water Conservation, 2005, 12(4): 59. [张小咏，刘耕年．冰川径流模型研究进展[J].水土保持研究，2005,12(4):59.]
[14] Khodakov V G. On the dependence of total ablation over the glacier surface on the air temperature [J]. Meteorol i Gidrol 1965, (7): 48-49.
[15] Krenke A N, Khodakov V G. On the relationship between the surface melting of glaciers with air temperature [J]. Materiality Glyatsiologicheskikh Issledovaniy Khronika Obsuzhdeniya 1966, (12): 153-162
[16] Ian C W illis Nell S A mold Ben W Brock Effect of snow pack removal on energy balance melt and runoff in a small supraglacial catchmen [J]. Hydrological Process 2002, (16): 1719-1750.
[17] Huang Xinhui Wang Zhangli Niu Zhenghua Main progress of research on hydrologic processes and prediction models [D]. Research of Soil and Water Conservation, 2004, 11(4): 107-108. [黄新会, 王占礼, 牛振华. 水文过程及模型研究主要进展 [D]. 水土保持研究, 2004, 11(4): 107-108.]
[18] Yang D, Sherath M, Musiake K. Comparison of different distributed hydrological models for characterization of catchment spatial variability [J]. Hydrological Processes 2000, 14: 405-413.
[19] Yu Xinying Liu Xinren Distributed hydrological model for water-sheds supplemented with melted snow and glacier water and rainfall [J]. Journal of Hohai University (Natural Sciences), 2002, 30(5): 24-26 [俞鑫颖, 刘新仁. 分布式冰雪融水雨水混合水文模型 [J]. 河海大学学报 (自然科学版), 2002, 30(5): 24-26 ]
[20] Turcotte R, Fortin JP. Determination of the drainage structure of a watershed using a digital elevation model and a digital river and lake network [J]. Journal of Hydrology, 2001, 240 (3-4): 225-242
[21] Zhen Hongxing Liu Changming Wang Zhonggeng Wu Xianfeng Simulation of basing hydrological processes in Huanghe Basin distributed hydrological mode [J]. Geographical Research, 2004, 23 (4): 452-453. [郑红星, 刘昌明, 王中根, 吴险峰. 黄河典型流域分布式水文过程模拟 [J]. 地理研究, 2004, 23 (4): 452-453.]

基于DEM的清水河分布式水文模型

Distributed hydrological model based on DEM in Qingshui River Basin

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