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    Evaluating CFSR and WATCH Data as Input to SWAT for the Estimation of the Potential Evapotranspiration in a Data-Scarce Eastern-African Catchment

    Source: Journal of Hydrologic Engineering:;2016:;Volume ( 021 ):;issue: 003
    Author:
    Tadesse Alemayehu
    ,
    Ann van Griensven
    ,
    Willy Bauwens
    DOI: 10.1061/(ASCE)HE.1943-5584.0001305
    Publisher: American Society of Civil Engineers
    Abstract: One of the key inputs of a hydrological model is the potential evapotranspiration (PET), which sets an upper limit to evapotranspirative water demand. However, limited data availability often challenges the choice of a PET estimation method, which in turn affects the PET estimates as well as the water balance (WB) components. The objectives of this research are (1) to evaluate the use of different sources of weather input data to derive PET: Climate Forecast System Reanalysis (CFSR) data, Water and Global Change (WATCH) data, and data generated by the weather generator of the soil and water assessment tool (SWAT) (SWAT–WG); and (2) to investigate the effects of the Penman–Monteith and Hargreaves (HG) methods on WB components using a SWAT-based model for the Upper Mara Catchment (Kenya). It is shown that PET estimations using the CFSR, WATCH, and SWAT–WG data sets compare well with the average annual and seasonal PET estimates from local observations over a period of 20 years. This shows the potential of global reanalysis climate data sources for the computation of PET in data-limited catchments. The SWAT models forced by these data sets and by gauged rainfall show a modified Nash–Sutcliffe (NSm) efficiency ranging from 0.6 to 0.72 for the simulation of the flow, depending on the selected PET estimation method. Unlike water yield, the other WB components simulated by the SWAT models (ET, deep aquifer loss, and reevaporation from the shallow aquifer) vary in magnitude, depending on the data and methods being used. The sensitivity analysis and the calibration results show that the model parameters are sensitive to the choice of the PET estimation method. Therefore, for catchments where parameterization is a challenge owing to data scarcity, it is crucial to consider the appropriate PET estimation method for a realistic modeling of the hydrological processes. In our case study, the HG method gives more robust and realistic ET estimations.
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      Evaluating CFSR and WATCH Data as Input to SWAT for the Estimation of the Potential Evapotranspiration in a Data-Scarce Eastern-African Catchment

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    contributor authorTadesse Alemayehu
    contributor authorAnn van Griensven
    contributor authorWilly Bauwens
    date accessioned2017-12-30T12:55:58Z
    date available2017-12-30T12:55:58Z
    date issued2016
    identifier other%28ASCE%29HE.1943-5584.0001305.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4243554
    description abstractOne of the key inputs of a hydrological model is the potential evapotranspiration (PET), which sets an upper limit to evapotranspirative water demand. However, limited data availability often challenges the choice of a PET estimation method, which in turn affects the PET estimates as well as the water balance (WB) components. The objectives of this research are (1) to evaluate the use of different sources of weather input data to derive PET: Climate Forecast System Reanalysis (CFSR) data, Water and Global Change (WATCH) data, and data generated by the weather generator of the soil and water assessment tool (SWAT) (SWAT–WG); and (2) to investigate the effects of the Penman–Monteith and Hargreaves (HG) methods on WB components using a SWAT-based model for the Upper Mara Catchment (Kenya). It is shown that PET estimations using the CFSR, WATCH, and SWAT–WG data sets compare well with the average annual and seasonal PET estimates from local observations over a period of 20 years. This shows the potential of global reanalysis climate data sources for the computation of PET in data-limited catchments. The SWAT models forced by these data sets and by gauged rainfall show a modified Nash–Sutcliffe (NSm) efficiency ranging from 0.6 to 0.72 for the simulation of the flow, depending on the selected PET estimation method. Unlike water yield, the other WB components simulated by the SWAT models (ET, deep aquifer loss, and reevaporation from the shallow aquifer) vary in magnitude, depending on the data and methods being used. The sensitivity analysis and the calibration results show that the model parameters are sensitive to the choice of the PET estimation method. Therefore, for catchments where parameterization is a challenge owing to data scarcity, it is crucial to consider the appropriate PET estimation method for a realistic modeling of the hydrological processes. In our case study, the HG method gives more robust and realistic ET estimations.
    publisherAmerican Society of Civil Engineers
    titleEvaluating CFSR and WATCH Data as Input to SWAT for the Estimation of the Potential Evapotranspiration in a Data-Scarce Eastern-African Catchment
    typeJournal Paper
    journal volume21
    journal issue3
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)HE.1943-5584.0001305
    page05015028
    treeJournal of Hydrologic Engineering:;2016:;Volume ( 021 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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