Influence of surface roughness in hydrological response of semiarid catchments

Abstract Here, an investigation has been carried out in order to understand the influence of the surface roughness in the definition of the hydrological response of semiarid catchments. Following a previous study of one of the authors, a modified version of TOPMODEL is used, in which the convolution routing procedure has been extended to the hillslopes by specifying the routing velocity for each pixel of the watershed. These velocities have been linked to the watershed land use through the different surface roughness whose coefficients has been derived on the basis of Engman's table. In this paper, roughness coefficient distributions are expressed as function of a unique value treated as a calibration parameter. An analysis of model response in terms of prediction has been made for each roughness coefficient distributions using the GLUE procedure. Results from the application of the modified version of TOPMODEL in a Mediterranean experimental catchment located in Sicily are presented and discussed.

[1]  Vijay P. Singh,et al.  Rainfall-runoff relationship , 1982 .

[2]  K. Beven,et al.  Toward a generalization of the TOPMODEL concepts:Topographic indices of hydrological similarity , 1996 .

[3]  Brent Clothier,et al.  Modelling the link between hillslope water movement and stream flow: application to a small Mediterranean forest watershed , 1997 .

[4]  K. Beven,et al.  A physically based, variable contributing area model of basin hydrology , 1979 .

[5]  Keith Beven,et al.  The sensitivity of hydrological models to spatial rainfall patterns: an evaluation using observed data , 1994 .

[6]  K. Beven,et al.  MODELLING THE HYDROLOGICAL RESPONSE OF MEDITERRANEAN CATCHMENTS, PRADES, CATALONIA. THE USE OF DISTRIBUTED MODELS AS AIDS TO HYPOTHESIS FORMULATION , 1997 .

[7]  A. Williams,et al.  Soil moisture variability in a semi-arid gully catchment: implications for runoff and erosion control , 1998 .

[8]  K. Beven,et al.  Testing a physically-based flood forecasting model (TOPMODEL) for three U.K. catchments , 1984 .

[9]  G. G. Pohlman Soil Science Society of America Proceedings , 1948, Soil Science Society of America Journal.

[10]  L. H. Cammeraat,et al.  The effect of land use on runoff and soil erosion rates under Mediterranean conditions , 1997 .

[11]  Edwin T. Engman,et al.  Roughness coefficients for routing surface runoff , 1983 .

[12]  A. Robson,et al.  Modelling the hydrology of submediterranean montane catchments (Mont-Lozère, France) using TOPMODEL: initial results , 1992 .

[13]  J. B. Thornes,et al.  Vegetation and erosion. Processes and environments. , 1992 .

[14]  P. Llorens,et al.  Studying the role of old agricultural terraces on runoff generation in a small Mediterranean mountainous basin , 1994 .

[15]  S. K. Jenson,et al.  Extracting topographic structure from digital elevation data for geographic information-system analysis , 1988 .

[16]  Rodger B.Grayson Ian D.Moore Effect Of Land-Surface Configuration On Catchment Hydrology , 1992 .

[17]  Keith Beven,et al.  Prophecy, reality and uncertainty in distributed hydrological modelling , 1993 .

[18]  J. Nash,et al.  River flow forecasting through conceptual models part I — A discussion of principles☆ , 1970 .

[19]  Juan Puigdefábregas,et al.  Effects of soil and vegetation on runoff along a catena in semi-arid Spain , 1996 .

[20]  Anthony J. Parsons,et al.  Overland Flow: Hydraulics and Erosion Mechanics , 2007 .

[21]  D. Maidment,et al.  UNIT HYDROGRAPH DERIVED FROM A SPATIALLY DISTRIBUTED VELOCITY FIELD , 1996 .

[22]  Keith Beven,et al.  The future of distributed models: model calibration and uncertainty prediction. , 1992 .

[23]  C. Gascuel-Odoux,et al.  Evolution of soil surface roughness and flowpath connectivity in overland flow experiments , 2002 .

[24]  Keith Beven Distributed hydrological modelling: applications of the TOPMODEL concept. , 1997 .

[25]  Keith Beven,et al.  Spatial and temporal predictions of soil moisture dynamics, runoff, variable source areas and evapotranspiration for plynlimon, mid-wales. , 1993 .

[26]  Ian D. Moore,et al.  A quasi-dynamic wetness index for characterizing the spatial distribution of zones of surface saturation and , 1994 .

[27]  The use of vegetation and land use parameters in modelling catchment sediment yields. , 1990 .

[28]  R. Bryan,et al.  Badland geomorphology and piping , 1984 .

[29]  Marco Franchini,et al.  Physical interpretation and sensitivity analysis of the TOPMODEL , 1996 .

[30]  Keith Beven,et al.  A dynamic TOPMODEL , 2001 .

[31]  M. Martínez-Mena,et al.  Factors influencing surface runoff generation in a Mediterranean semi-arid environment: Chicamo watershed, SE Spain , 1998 .