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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hess-15-3447-2011</article-id>
<title-group>
<article-title>Comparison of hydrological model structures based on recession and low flow simulations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Staudinger</surname>
<given-names>M.</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>Stahl</surname>
<given-names>K.</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>Seibert</surname>
<given-names>J.</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>Clark</surname>
<given-names>M. P.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tallaksen</surname>
<given-names>L. M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Geography, University of Zurich, Zurich, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Hydrology Freiburg, Albert-Ludwigs University, Freiburg, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University Cooperation for Atmospheric Research, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Geosciences, University of Oslo, Oslo, Norway</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>11</month>
<year>2011</year>
</pub-date>
<volume>15</volume>
<issue>11</issue>
<fpage>3447</fpage>
<lpage>3459</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 M. Staudinger et al.</copyright-statement>
<copyright-year>2011</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/15/3447/2011/hess-15-3447-2011.html">This article is available from https://hess.copernicus.org/articles/15/3447/2011/hess-15-3447-2011.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/15/3447/2011/hess-15-3447-2011.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/15/3447/2011/hess-15-3447-2011.pdf</self-uri>
<abstract>
<p>Low flows are often poorly reproduced by commonly used hydrological models,
which are traditionally designed to meet peak flow situations. Hence, there
is a need to improve hydrological models for low flow prediction. This study
assessed the impact of model structure on low flow simulations and recession
behaviour using the Framework for Understanding Structural Errors (FUSE).
FUSE identifies the set of subjective decisions made when building a
hydrological model and provides multiple options for each modeling decision.
Altogether 79 models were created and applied to simulate stream flows in the
snow dominated headwater catchment NarsjÃ¸ in Norway (119 km&lt;sup&gt;2&lt;/sup&gt;). All
models were calibrated using an automatic optimisation method. The results
showed that simulations of summer low flows were poorer than simulations of
winter low flows, reflecting the importance of different hydrological
processes. The model structure influencing winter low flow simulations is the
lower layer architecture, whereas various model structures were identified to
influence model performance during summer.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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