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干旱区地理 ›› 2003, Vol. 26 ›› Issue (1): 37-43.doi: 10.13826/j.cnki.cn65-1103/x.2003.01.007

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黑河干流山区流域月径流计算模型

陈仁升, 康尔泗, 杨建平, 王书功, 张济世   

  1. 中科院寒区旱区环境与工程研究所, 兰州 730000
  • 收稿日期:2002-01-16 修回日期:2002-09-20 发布日期:2025-12-31
  • 基金资助:
    中国科学院知识创新工程(编号:KZCX1-10-03-01)和中国科学院寒区旱区环境与工程研究所知识创新工程项目(编号:210036和210016)资助

MONTHLY RUNOFF MODEL IN MOUNTAINOUS REGION OF HEIHE MAINSTREAM RIVER

CHEN Ren-sheng, KANG Er-si, YANG Jian-ping, WANG Shu-gong, ZHANG Ji-shi   

  1. Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2002-01-16 Revised:2002-09-20 Online:2025-12-31

摘要: 西北内陆河山区流域天然来水量的准确预测对于维持区域可持续发展和生态环境的保护具有重大的意义。鉴于这些山区流域地形、地貌、植被景观复杂, 观测站点稀疏, 建立了6种月平均流量的计算模型, 效果都很好。所进行的数值试验表明, 山区平均月降水量、月平均气温、平均月蒸发量和出山月平均流量相互之间存在复杂的非线性关系。降水和气温都是影响月蒸发力和平均流量的一个综合因素。气温是影响含有冰雪融水的山区流域产流的一个极为重要的因素, 但降水、气温和蒸发力不足以完全综合反映产流过程, 应该探讨加入新的因子。

关键词: 黑河山区流域, 月平均流量, 月蒸发力, 月平均气温, 模型

Abstract: Water resource is very deficient in inland river basin of Northwest China. The runoff from mountainous watershed basically presents the regional water resources. How to simulate and predict the runoff from mountainous watershed is very important to the sustainable development and ecological environment protection of the inland river basin in Northwest China. However, these mountainous basins have complex topography, versatile ground feature, different landscape elements, while the meteorological and hydrological stations in these basins are relatively scare. Therefore, it is difficult to create highly precise distributed hydrological models and other models based on physical mechanism of runoff generation. Thus, in this paper, 6 empirical models for runoff generation have been created, which are classified into 2 types, the nonlinear statistical model and the artificial neural network model (ANN). All the models work well. The NSE of statistical model 1 is 0.8342 and 0.8094 for simulation and prediction process respectively, of statistical model 2 is 0.8115 and 0.8736 respectively, and of statistical model 3 is 0.8005 and 0.8748. The NSE of ANNs model 1 is 0.9033 and 0.7778, of model 2 is 0.8971 and 0.7708, of model 3 is 0.9809 and 0.8550.For simulation process, the ANNs models run better than the statistical models, while in the predicted process, the statistical model work better. From these numerical experiments, it can be conclude that the monthly averaged runoff, the monthly averaged air temperature, the monthly evaporation capacity and monthly precipitation have highly nonlinear relationship between each other. Precipitation and air temperature both are the comprehensive factors that effect the variation of the runoff and evaporation. Especially, for runoff generation in mountainous watershed with much ice, glacier and snow, the air temperature is a very important factor. However, precipitation, air temperature and evaporation capacity, in general, could not reflect the runoff generation process completely. Other factors that have important impacts should are found out.

Key words: mountainous watershed of Heihe River Basin, monthly averaged air temperature, monthly precipitation, monthly averaged runoff, models

中图分类号: 

  • P333.2