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<front>
<journal-meta>
<journal-id journal-id-type="publisher">HESS</journal-id>
<journal-title-group>
<journal-title>Hydrology and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">HESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hydrol. Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1607-7938</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hess-13-259-2009</article-id>
<title-group>
<article-title>Matching ERS scatterometer based soil moisture patterns with simulations of a conceptual dual layer hydrologic model over Austria</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Parajka</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Naeimi</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Blöschl</surname>
<given-names>G.</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>Komma</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Hydraulic and Water Resources Engineering, Vienna University of Technology, Austria</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Austria</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Hydrology, Slovak Academy of Sciences, Bratislava, Slovakia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>02</month>
<year>2009</year>
</pub-date>
<volume>13</volume>
<issue>2</issue>
<fpage>259</fpage>
<lpage>271</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 J. Parajka et al.</copyright-statement>
<copyright-year>2009</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/articles/13/259/2009/hess-13-259-2009.html">This article is available from https://hess.copernicus.org/articles/13/259/2009/hess-13-259-2009.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/13/259/2009/hess-13-259-2009.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/13/259/2009/hess-13-259-2009.pdf</self-uri>
<abstract>
<p>This study compares ERS scatterometer top soil moisture observations with
simulations of a dual layer conceptual hydrologic model. The comparison is
performed for 148 Austrian catchments in the period 1991–2000. On average,
about 5 to 7 scatterometer images per month with a mean spatial coverage of
about 37% are available. The results indicate that the agreement between
the two top soil moisture estimates changes with the season and the weight
given to the scatterometer in hydrologic model calibration. The hydrologic
model generally simulates larger top soil moisture values than are observed
by the scatterometer. The differences tend to be smaller for lower altitudes
and the winter season. The average correlation between the two estimates is
more than 0.5 in the period from July to October, and about 0.2 in the
winter months, depending on the period and calibration setting. Using both
ERS scatterometer based soil moisture and runoff for model calibration
provides more robust model parameters than using either of these two sources
of information.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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