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    <titleInfo>
      <title>Hydrological performance of the ERA5 reanalysis for flood modeling in Tunisia with the LISFLOOD and GR4J models</title>
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      <namePart type="family">Cantoni</namePart>
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    <abstract>Study region: This study is focused on 6 catchments in Tunisia, in North Africa, under a semi-arid climate where daily river discharge and precipitation observations are available between 1992 and 2006.Study focus: The distributed hydrological model LISFLOOD has been compared with a lumped model, GR4J, to reproduce river runoff and floods, using observed rainfall interpolated from rain gauges and from the ERA5 reanalysis.New hydrological insights for the region under study: LISFLOOD and GR4J with their default pa-rameters have little skill in Tunisia, but when calibrated, both hydrological models provide similar performance to reproduce river discharge,with a mean KGE of 0.65 for GR4J driven by observed rainfall, and 0.59 with ERA5, and similarly a mean KGE of 0.59 for LISFLOOD driven by observed rainfall and 0.48 with ERA5. All model simulations perform very similarly using either observed rainfall data from rain gauges inter-polated over the basins or ERA5 rainfall, indicating its value as an alternative to observations in data-scarce areas such as Tunisia. The development of regional databases of river discharge ob-servations in North Africa could allow the calibration of such hydrological models on a larger scale for operational flood modeling and forecasting.</abstract>
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    <subject>
      <topic>Floods</topic>
      <topic>Tunisia</topic>
      <topic>LISFLOOD</topic>
      <topic>EFAS</topic>
      <topic>GR4J</topic>
      <topic>ERA5</topic>
    </subject>
    <subject authority="local">
      <geographic>TUNISIE</geographic>
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    <classification authority="local">062</classification>
    <classification authority="local">020</classification>
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      <titleInfo>
        <title>Journal of Hydrology : Regional Studies</title>
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      <part>
        <detail type="volume">
          <number>42</number>
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        <extent unit="pages">
          <list> 101169 [15 p.]</list>
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      <originInfo>
        <dateIssued>2022</dateIssued>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010085962</identifier>
    <identifier type="doi">10.1016/j.ejrh.2022.101169</identifier>
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      <recordCreationDate encoding="w3cdtf">2022-09-28</recordCreationDate>
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