APPLICATION OF A CONCEPTUAL HYDROLOGICAL MODEL IN THE RUNOFF FORECAST OF A MOUNTAINOUS WATERSHED
Received date: 2001-03-28
Revised date: 2001-06-13
Online published: 2002-02-01
Based on the basic principle of the HBV conceptual hydrological model, a hydrological model of the mountainous watersheds in the arid inland area of northwest China was developed by the authors. This model reflects the characteristics of the runoff generation in the mountainous watersheds of west China. The model simulates the runoff formation and transformation processes of the mountainous watersheds by dividing the watersheds into two basic altitude zones, the high mountain ice and snow zone and the mountain vegetation zone. Taking the monthly air temperature and precipitation of the standard meteorological stations as the foremost inputs to the model, the monthly runoff from the mountainous watersheds is then simulated. The model is applied to simulate the water balance of a mountainous watershed of the Heihe River basin at the north flank of the Qilian mountains, and the annual runoff and its monthly distribution is then forecasted. The results indicate that, from the dry years to the we years, all of the precipitation, evaporation, runoff and runoff coefficient increase, but the alimentation proportion of glacial meltwater and snow meltwater to the total runoff decrease. Therefore, the ice and snow meltwater plays a regulation function for the runoff. In the mountainous watershed of the Heihe River, the runoff coefficient is much larger than that of the whole arid area, but it is still less than the average value over the whole country. The model of runoff simulation and forecast for the inland mountainous watersheds applied in the present study shows rather good fitness in the forecast of the annual runoff and its monthly distribution. Therefore, the model can be used for the runoff forecast of the mountainous watersheds both of the Heihe River and other inland rivers of the arid area of northwest China. And this will serve the rational allocation, utilization and exploitation of water resources in the middle and down courses of the inland river basins.
KANG Ersi,CHENG Guodong,LAN Yongchao,CHEN Rensheng,ZHANG Jishi . APPLICATION OF A CONCEPTUAL HYDROLOGICAL MODEL IN THE RUNOFF FORECAST OF A MOUNTAINOUS WATERSHED[J]. Advances in Earth Science, 2002 , 17(1) : 18 -26 . DOI: 10.11867/j.issn.1001-8166.2002.01.0018
[1] Bergstrom S. Development and Application of a Conceptual Runoff model for Scandinavian Catchments[C]. Bulletin Series A, No 52, Lund: Lund University, 1976.12-83.
[2] Kang Ersi, Cheng Guodong, Lan Yongchao, et al. A model for simulating the response of runoff from the mountainous watersheds of inland river basins in the arid area of northwest China to climate changes[J]. Science in China (Series D), 1999, 42(Suppl): 52-63. [康尔泗,程国栋,蓝永超,等. 西北干旱区内陆河流域出山径流变化趋势对气候变化响应模型[J]. 中国科学(D辑),1999,29(Supp.1):48-54.]
[3] Yang Daqing, Shi Yafeng, Kang Ersi, et al. Analysis and correction of systematic errors in precipitation measurement in the Urumuqi River basin, Tianshan[A]. In: Shi Yafeng, et al, eds. Formation and Estimation of Mountain Water Resources in the Urumqi River Basin[C]. Beijing: Science Press, 1992. 14-40. [杨大庆,施雅风,康尔泗,等. 天山乌鲁木齐河流域降水观测系统误差分析和修正[A]. 见:施雅风,等编. 乌鲁木齐河山区水资源形成和估算[C]. 北京:科学出版社,1992. 14-40.]
[4] Kang Ersi, Atsumu Ohmura. Energy, water and mass balance and runoff models in Tianshan glacieraffected area[J]. Science in China (Series B), 1994, 24(9): 983-991. [康尔泗,Ohmura A. 天山冰川作用流域能量、水量和物质平衡及径流模型[J]. 中国科学(B辑),1994,24(9):983-991.]
[5] Kang Ersi. Energy-water-mass Balance and Hydrological Discharge[M]. Zurcher Geographische Schriften 57. Zurich: ETH, 1994. 45-99.
[6] Braun L N. Simulation of Snowmelt-runoff in Lowland and Lower Alpine Regions of Switzerland[M]. Zurcher Geographische Schriften 21. Zurich:ETH, 1985. 1-50.
[7] Braun L N, Grabs W,Rana B. Application of a conceptual precipitationrunoff model in the Langtang Khola Basin, Nepal Himalaya[J]. IAHS Publ, 1993, No. 218: 221-237.
[8] Kang Ersi,Ohmura A. A parameterized energy balance model of glacier melting on the Tianshan mountain[J]. Acta Geographica Sinica, 1994, 49(5): 467-476.[康尔泗,Ohmura A. 天山冰川消融参数化能量平衡模型[J]. 地理学报, 1994, 49(5):467-476.]
[9] Tan Guanri, Yan Jiyuan, Zhu Ruizhao. Applied climatology[M]. Shanghai: Shanghai Science and Technology Press, 1985. 194-195. [谭冠日, 严济远,朱瑞兆. 应用气候[M]. 上海:上海科学技术出版社,1985.194-195.]
[10] Zhang Guowei, Maire Yanmu. Estimation of evaporation and its characteristics analysis in the mountainous area of the Urumqi River basin[A]. In: Shi Yafeng, et al, eds. Formation and estimation of Mountain Water Resources in the Urumqi River Basin[C]. Beijing: Science Press, 1992. 90-98.[张国威,买热艳木. 乌鲁木齐河山区流域蒸发估算及特征分析[A]. 见:施雅风等,编. 乌鲁木齐河山区水资源形成和估算[C]. 北京: 科学出版社,1992.90-98.]
[11] Editorial Board of “Physical geography of China”, Chinese Academy of Sciences. Physical Geography of China (Surface Water)[M]. Beijing: Science Press, 1981.[中国科学院《中国自然地理》编辑委员会. 中国自然地理(地表水)[M]. 北京:科学出版社,1981.]
/
〈 |
|
〉 |