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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-6-899-2002</article-id>
<title-group>
<article-title>Improved unit hydrograph characterisation of the daily flow regime (including low flows) for the River Teifi, Wales: towards better rainfall-streamflow models for regionalisation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Littlewood</surname>
<given-names>I.G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Centre for Ecology and Hydrology, Wallingford, OXON, OX10 8BB</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Email: igl@ceh.ac.uk</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>10</month>
<year>2002</year>
</pub-date>
<volume>6</volume>
<issue>5</issue>
<fpage>899</fpage>
<lpage>911</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2002 I.G. Littlewood</copyright-statement>
<copyright-year>2002</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://hess.copernicus.org/articles/6/899/2002/hess-6-899-2002.html">This article is available from https://hess.copernicus.org/articles/6/899/2002/hess-6-899-2002.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/6/899/2002/hess-6-899-2002.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/6/899/2002/hess-6-899-2002.pdf</self-uri>
<abstract>
<p>An established rainfall-streamflow
modelling methodology employing a six-parameter unit hydrograph-based
rainfall-runoff model structure is developed further to give an improved
model-fit to daily flows for the River Teifi at Glan Teifi. It is shown that a
previous model of this type for the Teifi, which (a) accounted for 85% of the
variance in observed streamflow, (b) incorporated a pure time delay of one day
and (c) was calibrated using a trade-off between two model-fit statistics (as
recommended in the original methodology), systematically over-estimates low
flows. Using that model as a starting point the combined application of a
non-integer pure time delay and further adjustment of a temperature modulation
parameter in the loss module, using the flow duration curve as an additional
model-fit criterion, gives a much improved model-fit to low flows, while leaving
the already good model-fit to higher flows essentially unchanged. The further
adjustment of the temperature modulation loss module parameter in this way is
much more effective at improving model-fit to low flows than the introduction of
the non-integer pure time delay. The new model for the Teifi accounts for 88% of
the variance in observed streamflow and performs well over the 5 percentile to
95 percentile range of flows. Issues concerning the utility and efficacy of the
new model selection procedure are discussed in the context of hydrological
studies, including regionalisation.&lt;/p&gt;
&lt;p style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords:&lt;/b&gt; unit hydrographs, rainfall-runoff modelling, low flows, regionalisation.&lt;/p&gt;</p>
</abstract>
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