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地貌气候瞬时单位线数学模型及其应用
引用本文:黄晶,胡振鹏.地貌气候瞬时单位线数学模型及其应用[J].南昌大学学报(工科版),1992(1).
作者姓名:黄晶  胡振鹏
作者单位:北京市水利规划设计研究院,江西工业大学
摘    要:本文系统地归纳与介绍了基于随机理论的现代汇统计算方法——地貌气候瞬时单位线理论,在对该单位线理论进行概率释义的基础上建立了四级河网流域的地貌气候瞬时单位线数学模型。在模型建立过程中进行了严密的数学推导,对模型中各参数的定义及求算方法也作了详细说明。最后本文以安徽省滁州径流实验流域为例进行了参数求算、单位线确定和汇流计算。通过比较流域出口断面的计算洪水流量过程和实测洪水流量过程验证了地貌气候瞬时单位线数学模型的有效性。

关 键 词:响应函数  Strahler分级系统  马尔科夫链  转移概率  初始概率  滞留时间的倒数  卷积

MOdel of GeomorPho-Climatic Instantaneous Unit Hydrogrograph aud its Applicatiou
Huang Jing.MOdel of GeomorPho-Climatic Instantaneous Unit Hydrogrograph aud its Applicatiou[J].Journal of Nanchang University(Engineering & Technology Edition),1992(1).
Authors:Huang Jing
Affiliation:Huang Jing (Beijing Institute of Planniug aud Desiguing for Water Resourles) Hu Zheupeug (Jiaugxi Polytechnic University)
Abstract:On the basis of the stochastic theory, a modern watershed flow concentration method-Geomorpho-Climatic Instantaneous Unit Hydrograph (G. C. IUH) Theory-is introduced systemly in this paper. We set up a 4-order river system G. C. IUH model ba ed on the probability explanation of G. C. IUH after the strictly mathematical deduction. This paper also provides the parameters definition and calculation method in the model. We take the Chuzhou Experimental Basin in Anhui Province as an example to determine the G. C. IUH and predict the flood processes at the basin outlet. The effect of model is testified by the comparison between the calculated result and observed result.
Keywords:response function  Strahler Ordering System  Markov Chain  transition probability  initial probability  inverse of waiting time  Convolution
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