<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Estimation of actual evapotranspiration over a rainfed vineyard using a 1-D water transfer model : A case study within a Mediterranean watershed</dc:title>
  <dc:creator>Galleguillos, M.</dc:creator>
  <dc:creator>/Jacob, Fr&#xE9;d&#xE9;ric</dc:creator>
  <dc:creator>Prevot, L.</dc:creator>
  <dc:creator>Faundez, C.</dc:creator>
  <dc:creator>Bsaibes, A.</dc:creator>
  <dc:subject>Heterogeneous landscape</dc:subject>
  <dc:subject>HYDRUS-1D</dc:subject>
  <dc:subject>Vadose zone</dc:subject>
  <dc:subject>Water table</dc:subject>
  <dc:description>The current study aims to evaluate the capabilities of soil water balance modeling to estimate ET for very different conditions of rainfed grapevine water status, within a vineyard landscape that depicts heterogeneities in canopy, soil and water table conditions. We calibrated the HYDRUS-1D model against measurements of the soil moisture profile within seven contrasted sites, we validated HYDRUS-1D sim-ulations against ET estimates derived from eddy covariance (EC) measurements within two contrasted sites, and we analyzed the temporal dynamics of the HYDRUS-1D ET simulations throughout almost two growth cycles for the seven sites. The calibration of HYDRUS-1D was correctly achieved, with a relative RMSE of 20% on average. Validation of HYDRUS-1D simulations against EC measurements was satisfactory, with RMSE values of about 40W m(-2) at the hourly timescale and 0.5 mm d(-1) at the daily timescale. HYDRUS-1D was able to provide consistent time series of ET within the seven contrasted sites and throughout the two growth cycles. We conclude that HYDRUS-1D simulations can be used as an alternative to EC measurements within rainfed vineyards, to alleviate experimental efforts for device cost and maintenance. Further, HYDRUS-1D simulations can be used for characterizing spatial variabili-ties and temporal dynamics, assessing impact of pedological conditions and land use on ET, or validating remote sensing retrievals over regional extents.</dc:description>
  <dc:date>2017</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010069474</dc:identifier>
  <dc:identifier>fdi:010069474</dc:identifier>
  <dc:identifier>Galleguillos M., Jacob Fr&#xE9;d&#xE9;ric, Prevot L., Faundez C., Bsaibes A.. Estimation of actual evapotranspiration over a rainfed vineyard using a 1-D water transfer model : A case study within a Mediterranean watershed. 2017, 184,  67-76</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>FRANCE</dc:coverage>
</oai_dc:dc>
