Abstract

This study was conducted for parametres estimation and stream flow prediction at ungauged catchments on the case of Upper Tekeze basin, Ethiopia by using Rainfall-runoff model. In the basin, most of the catchments were ungauged. The basin has 9199km2 and 3638km2 gauged and ungauged catchments respectively. Rainfall and stream flow data were analyzed in the period of 1992-2006 and 1992-20006, respectively. Parameters calibrated for gauged catchments were extrapolated to ungauged catchments on the base of similar physical catchment characteristics using regionalization techniques. Regionalization methods such as multiple linear regression, spatial proximity, sub basin mean and area ratio were applied to transfer model parameters values from gauged to ungauged catchments. For this study seven gauged catchments were satisfied objective functions in the calibrated and validation period, for example in Gheba catchment Nash-Sutcliffe model efficiency coefficient (NSE), relative volume error (RVE) and coefficient of determination (R2) were, 0.81, -4.25, 0.77 and 0.71, 5.5, 0.74 respectively. Stream flow simulation at ungauged catchments by using spatial proximity and sub basin mean method were contributing high runoff volume compare to other methods. The result for this study shows that the Key model parameters like runoff coefficient (Beta), recession coefficient of upper reservoir zone (Khq), Limit for evapotranspiration (Lp), field capacity (Fc), percolation (Perc) as defaulting value when applying HBV-96 model to the future regionalization studies. Model parameters were calibrated manually by try and error rules, however it was tidies therefore more creative automatic model calibration techniques could be useful for upcoming studies. Thus, Current and future water resources development endeavors may use apply such discharge data for planning and design purposes.

Highlights

  • Hydrological data are energetic for assessment of water resources problems, most of Ethiopian river basins are ungauged

  • The situation in Upper Tekeze basin is more challenging there is no evenly distributed hydrometric stations and large areas have a lack of gauged stations and only a few years of data are available and recorded

  • The model performance of Emba Mader watershed by HBV-96 model are satisfactory with objective functions like Nash-Sutcliffe model efficiency coefficient (NSE)=0.7, coefficient of determination (R2)=0.8, relative volume error (RVE)=4.8 and Nash-Sutcliffe model efficiency coefficient (NSE)=0.88, coefficient of determination (R2) =0.74, relative volume error (RVE)=-4.1 for the calibration and validation period respectively

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Summary

Introduction

Hydrological data are energetic for assessment of water resources problems, most of Ethiopian river basins are ungauged. Recorded and not well managed hydrological data that causes failurty of most water and civil structures. This scarce hydrological data results uncertainty both in design and management of water resources system [11]. Models are used as utility of water resources development, in assessing and analyzing the available water resources, in studying the impacts of human interference in an area such as land use land cover change, deforestation and other hydraulics structures such as dams and reservoirs [10]. Understanding the basic relationships between rainfall-runoff, soil moisture, ground water level and land use land cover is vital for an effective and sustainable water resources planning and management activities with the support of models [14]

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