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一种基于面积-时间关系的单位线分析方法 被引量:12

A Method Deriving Unit Hydrographs Based on Area-Time Relation
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摘要 为了分析分布或半分布式水文模型计算单元的单位线,提出了一种基于面积-时间关系的单位线分析方法.首先利用数字高程模型(DEM)分析计算面积-时间关系,然后将其转换为流量-时间关系.考虑到流域对径流的调蓄作用,利用线性水库将流量-时间关系转换成单位线.将分析的单位线用于HEC-HMS并在沿渡河流域进行实例应用,结果表明,模拟过程与实测过程拟合较好.提出的方法可用于分析无资料流域的汇流单位线. A method to derive unit hydrographs for sub-areas of distributed model based on area-time relation was proposed. The area-time histograms derived by means of digital elevation model(DEM) were translated to discharge-time histograms. In order to model the store and delay effect of watersheds on flow, the discharge-time histograms were routed through a linear reservoir and unit hydrographs were obtained. Application of HEC-HMS, in which unit hydrographs were used, in Yandu river watershed was performed. The results show that the simulated flood hydrographs is coincident with the observed ones. The method presented can be used to derive unit hydrographs for ungaged watersheds.
出处 《中国矿业大学学报》 EI CAS CSCD 北大核心 2007年第3期356-359,共4页 Journal of China University of Mining & Technology
基金 中国矿业大学科技基金项目(OF4533)
关键词 单位线 面积-时间关系 数字高程模型 HEC—HMS unit hydrograph area-time relation DEM HEC-HMS
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参考文献7

  • 1RODRIGUEZ-ITUSBE I,VALDES J B.The geomorphological structure of hydrologic response[J].Water Resources Research,1979,15(6):1409-1420.
  • 2AJWARD M H,MUZIK I.A spatially varied unit hydrograph model[J].Journal of Environmental hydrology,2000(8):7-15.
  • 3詹道江,叶守泽.工程水文学[M].北京:中国水利水电出版社,2003:94.
  • 4CLARK C O.Storage and the unit hydrograph[J].Transaction American Society of Civil Engineers,1945,110:1419-1446.
  • 5MAIDMENT D R.Unit hydrograph derived from a spatially distributed velocity field[J].Hydrological Processes,1996,10:831-844.
  • 6FAIRCHILD J,LEYMARIE P.Drainage networks from grid digital elevation models[J].Water Resources Research,1991,27(5):709-717.
  • 7孔凡哲,李莉莉.数字高程模型在新安江模型中的应用研究[J].中国矿业大学学报,2006,35(3):393-396. 被引量:12

二级参考文献9

  • 1QUINN P F, BEVEN K J, PLANCHON O. The prediction of.hillslope flow path for distributed hydrological modeling using digital terrain model [J],Hydrological Processes, 1991,5 :59-79.
  • 2QUINN P F, BEVEN K J, LAMB R. The In(a/tanβ) index: how to calculate it and how to use it in the TOPMODEL framework [J]. Hydrological Processes. 1995.(9):161-185.
  • 3ABBOTT M B, BATHURST J C, CUNGE J A , et al. An introduction to the European Hydroloic System-Systeme Hydrologique Europeen, SHE, 1: History and philosophy of a physically-based, distributed modeling system[J]. Journal of Hydrology, 1086,87:45 -59.
  • 4ABBOTT M B, BATHURST J C, CUNGE J A , et al. An introduction to the European Hydroloic System-Systeme Hydrologique Europeen, SHE, 2:structure of a physically based, distributed modeling system [J]. Journal of Hydrology, 1986,87:61-77.
  • 5BEVEN K J, KIRKBY M J. A physically-based,variable contributing area model of basin hydrology [J]. Hydrological Sciences Bulletin. 1979,24 : 43-69.
  • 6GARROTE L, BRAS R L, A distributed model for real-time flood forecasting using digital elevation models[J]. Journal of Hydrology, 1995, 167: 279-306.
  • 7郝振纯 苏凤阁.分布式月水文模型研究及在淮河流域的应用[J].水科学进展,2000,11:36-36.
  • 8李致家,孔祥光,张初旺.对新安江模型的改进[J].水文,1998,17(4):19-23. 被引量:35
  • 9周买春,A.W.Jayawardena.利用双抛物线型土壤蓄水容量曲线对新安江产流模型的改进[J].水利学报,2002,33(12):38-43. 被引量:15

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