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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" 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:contributor>Prasanna H. Gowda</dc:contributor>
  <dc:contributor>Michael Hobbins</dc:contributor>
  <dc:contributor>Gabriel B. Senay</dc:contributor>
  <dc:contributor>George Paul</dc:contributor>
  <dc:contributor>Thomas Marek</dc:contributor>
  <dc:contributor>Dana Porter</dc:contributor>
  <dc:creator>Jerry Moorhead</dc:creator>
  <dc:date>2015</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The National Oceanic and Atmospheric Administration (NOAA) provides daily reference evapotranspiration (ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt;) maps for the contiguous United States using climatic data from North American Land Data Assimilation System (NLDAS). This data provides large-scale spatial representation of ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt;, which is essential for regional scale water resources management. Data used in the development of NOAA daily ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt; maps are derived from observations over surfaces that are different from short (grass — ET&lt;/span&gt;&lt;sub&gt;os&lt;/sub&gt;&lt;span&gt;) or tall (alfalfa — ET&lt;/span&gt;&lt;sub&gt;rs&lt;/sub&gt;&lt;span&gt;) reference crops, often in nonagricultural settings, which carries an unknown discrepancy between assumed and actual conditions. In this study, NOAA daily ET&lt;/span&gt;&lt;sub&gt;os&lt;/sub&gt;&lt;span&gt; and ET&lt;/span&gt;&lt;sub&gt;rs&lt;/sub&gt;&lt;span&gt; maps were evaluated for accuracy, using observed data from the Texas High Plains Evapotranspiration (TXHPET) network. Daily ET&lt;/span&gt;&lt;sub&gt;os&lt;/sub&gt;&lt;span&gt;, ET&lt;/span&gt;&lt;sub&gt;rs&lt;/sub&gt;&lt;span&gt; and the climatic data (air temperature, wind speed, and solar radiation) used for calculating ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt; were extracted from the NOAA maps for TXHPET locations and compared against ground measurements on reference grass surfaces. NOAA ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt;maps generally overestimated the TXHPET observations (1.4 and 2.2&amp;nbsp;mm/day ET&lt;/span&gt;&lt;sub&gt;os&lt;/sub&gt;&lt;span&gt; and ET&lt;/span&gt;&lt;sub&gt;rs&lt;/sub&gt;&lt;span&gt;, respectively), which may be attributed to errors in the NLDAS modeled air temperature and wind speed, to which reference ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt; is most sensitive. Therefore, a bias correction to NLDAS modeled air temperature and wind speed data, or adjustment to the resulting NOAA ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt;, may be needed to improve the accuracy of NOAA ET&lt;/span&gt;&lt;sub&gt;ref&lt;/sub&gt;&lt;span&gt; maps.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/1752-1688.12303</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>Accuracy assessment of NOAA gridded daily reference evapotranspiration for the Texas High Plains</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>