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    <titleInfo>
      <title>Reliability of SM2RAIN precipitation datasets in comparison to gauge observations and hydrological modelling over arid regions</title>
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    <abstract>Numerous satellite-based precipitation datasets have been successively made available. Their precipitation estimates rely on clouds properties derived from microwave and thermal sensors in a so-named 'top-down' approach. Recently, a 'bottom-up' approach to infer precipitation from soil moisture (SM) estimates has resulted in the release of two new precipitation datasets (P-datasets). One uses satellite-based SM estimates from the European Spatial Agency (ESA) Climate Change Initiative (CCI) (SM2RAIN-CCI) while the other uses satellite-based SM from European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) Advanced SCATterometer (ASCAT) (SM2RAIN-ASCAT). This study assesses SM2RAIN-ASCAT and -CCI reliability over two arid regions: Bolivian and Peruvian Altiplano and Pakistan (South Asia) using (a) direct comparisons with rain gauges and (b) testing the sensitivity of streamflow modelling to the P-datasets. Selecting two different regions and different indicators helps to assess whether the P-dataset reliability varies depending on the assessment method and location. For comparison purposes, the most reliable P-datasets from the literature are also considered (IMERG-E v.6, IMERG-L v.6, IMERG-F v.6, CHIRPS v.2 and MSWEP v.2.2). Compared to rain gauge observations and based on the modified Kling-Gupta Efficiency (KGE) values, the SM2RAIN-ASCAT and -CCI are more accurate in the Altiplano than in Pakistan. This difference is explained by a more favourable physical context for satellite-based SM estimates in the Altiplano. Over the Altiplano and despite an overall positive bias, SM2RAIN-ASCAT describes rain gauges temporal dynamics as well as IMERG-F v.6, CHIRPS v.2 and MSWEP v.2.2 and provides streamflow simulations very close to those obtained when using IMERG-F v.6, CHIRPS v.2 and MSWEP v.2.2 as forcing data.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>arid region</topic>
      <topic>assessment</topic>
      <topic>gauges</topic>
      <topic>hydrological modelling</topic>
      <topic>satellite</topic>
      <topic>precipitation</topic>
      <topic>SM2RAIN</topic>
    </subject>
    <subject authority="local">
      <geographic>ZONE ARIDE</geographic>
      <geographic>BOLIVIE</geographic>
      <geographic>PEROU</geographic>
      <geographic>PAKISTAN</geographic>
    </subject>
    <classification authority="local">062</classification>
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      <titleInfo>
        <title>International Journal of Climatology</title>
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      <part>
        <detail type="volume">
          <number>41</number>
        </detail>
        <detail type="volume">
          <number>suppl. 1</number>
        </detail>
        <extent unit="pages">
          <list>E517-E536</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2021</dateIssued>
      </originInfo>
      <identifier type="issn">0899-8418</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010079415</identifier>
    <identifier type="doi">10.1002/joc.6704</identifier>
    <identifier type="issn">0899-8418</identifier>
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      <url access="row object">https://www.documentation.ird.fr/intranet/publi/2020/08/010079415.pdf</url>
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      <recordCreationDate encoding="w3cdtf">2020-09-17</recordCreationDate>
      <recordChangeDate encoding="w3cdtf">2025-02-24</recordChangeDate>
      <recordIdentifier>fdi:010079415</recordIdentifier>
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