A parsimonious geomorphological unit hydrograph for rainfall-runoff modelling in small ungauged basins

被引:179
作者
Grimaldi, S. [1 ,2 ,3 ]
Petroselli, A. [4 ]
Nardi, F. [2 ]
机构
[1] Univ Tuscia, DIBAF Dept, I-01100 Viterbo, Italy
[2] Univ Roma La Sapienza, Honors Ctr Italian Univ H2CU, I-00184 Rome, Italy
[3] NYU, MetroTech Ctr 6, Polytech Inst, Dept Mech & Aerosp Engn, Brooklyn, NY 11201 USA
[4] Univ Tuscia, Dipartimento Sci & Tecnol Agr Foreste Nat & Energ, I-01100 Viterbo, Italy
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 2012年 / 57卷 / 01期
关键词
rainfall-runoff models; GIS; GIUH; WFIUH; DEM; terrain analysis; unit hydrograph; ungauged basin; small basin; DIGITAL ELEVATION MODELS; HYDROLOGIC RESPONSE; KINEMATIC DISPERSION; CATCHMENTS; WILDFIRES;
D O I
10.1080/02626667.2011.636045
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In this study, a parsimonious hydrological modelling algorithm is proposed based on the automated DEM-based geomorphic characterization of runoff dynamics in scarcely monitored river basins. The proposed approach implements the instantaneous unit hydrograph (IUH) concept, estimated using the width function (WF), for characterizing the travel time distribution using just one parameter, the river network flow velocity. Hillslope velocities are defined using spatially-distributed empirical formulas based on slope and soil-use information extrapolated from digital topographic data. Case studies are presented for testing model performance and comparing simulated and observed hydrographs of 25 selected flood events, as well as investigating the differences with the geomorphological instantaneous unit hydrograph (GIUH) model results. The calibration of the WFIUH channel flow velocity parameter using the concentration time is investigated providing interesting insights for the use of such a method for hydrological prediction in ungauged basins.
引用
收藏
页码:73 / 83
页数:11
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