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<front>
<journal-meta>
<journal-id journal-id-type="publisher">HESSD</journal-id>
<journal-title-group>
<journal-title>Hydrology and Earth System Sciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">HESSD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hydrol. Earth Syst. Sci. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1812-2116</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hessd-10-9999-2013</article-id>
<title-group>
<article-title>Modeling insights from distributed temperature sensing data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Buck</surname>
<given-names>C. R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Null</surname>
<given-names>S. E.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Butte County Department of Water and Resource Conservation, Oroville, California, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Watershed Sciences, Utah State University, Utah, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>08</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>8</issue>
<fpage>9999</fpage>
<lpage>10034</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 C. R. Buck</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://hess.copernicus.org/preprints/10/9999/2013/hessd-10-9999-2013.html">This article is available from https://hess.copernicus.org/preprints/10/9999/2013/hessd-10-9999-2013.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/preprints/10/9999/2013/hessd-10-9999-2013.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/preprints/10/9999/2013/hessd-10-9999-2013.pdf</self-uri>
<abstract>
<p>Distributed Temperature Sensing (DTS) technology can collect
  abundant high resolution river temperature data over space and time
  to improve development and performance of modeled river
  temperatures. These data can also identify and quantify thermal
  variability of micro-habitat that temperature modeling and standard
  temperature sampling do not capture. This allows researchers and
  practitioners to bracket uncertainty of daily maximum and minimum
  temperature that occurs in pools, side channels, or as a result of
  cool or warm inflows. This is demonstrated in a reach of the Shasta
  River in Northern California that receives irrigation runoff and
  inflow from small groundwater seeps. This approach highlights the
  influence of air temperature on stream temperatures, and indicates
  that physically-based numerical models may under-represent this
  important stream temperature driver. This work suggests DTS datasets
  improve efforts to simulate stream temperatures and demonstrates the
  utility of DTS to improve model performance and enhance detailed
  evaluation of hydrologic processes.</p>
</abstract>
<counts><page-count count="36"/></counts>
</article-meta>
</front>
<body/>
<back>
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