<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0188-6266</journal-id>
<journal-title><![CDATA[Acta universitaria]]></journal-title>
<abbrev-journal-title><![CDATA[Acta univ]]></abbrev-journal-title>
<issn>0188-6266</issn>
<publisher>
<publisher-name><![CDATA[Universidad de Guanajuato, Dirección de Investigación y Posgrado]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0188-62662019000100185</article-id>
<article-id pub-id-type="doi">10.15174/au.2019.2187</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Calibración de un modelo lluvia-escorrentía combinando la optimización manual y automática para un sistema de alta montaña]]></article-title>
<article-title xml:lang="en"><![CDATA[Calibration of a conceptual rainfall-runoff model combining manual and automatic optimization for high mountain systems]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Orozco]]></surname>
<given-names><![CDATA[Ismael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ramírez]]></surname>
<given-names><![CDATA[Aldo I.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Francés]]></surname>
<given-names><![CDATA[Félix]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Guanajuato Departamento de Ingeniería Geomática e Hidráulica ]]></institution>
<addr-line><![CDATA[Guanajuato Gto.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Tecnológico de Monterrey Escuela de Ingeniería y Ciencias ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universitat Politècnica de València Instituto de Ingeniería del Agua y Medio Ambiente ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>España</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>29</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0188-62662019000100185&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0188-62662019000100185&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0188-62662019000100185&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La calibración de un modelo lluvia-escorrentía es un proceso complicado que puede llevar mucho tiempo y esfuerzo. Su éxito está condicionado a la experiencia del modelador y al conocimiento que se tenga del sistema físico que se desea modelar. Por ello, en este trabajo, se propone una metodología que combina la calibración manual y automática para obtener los parámetros efectivos de un modelo hidrológico aplicado a una cuenca de alta montaña. Lo anterior se debe a que calibrar simultáneamente los parámetros hidrológicos y los parámetros de fusión de nieve puede no representar adecuadamente las condiciones reales de los sistemas de alta montaña. La metodología propuesta ha sido probada usando el modelo hidrológico distribuido TETIS desarrollado en la Universitat Politècnica de València. Los resultados obtenidos son buenos al alcanzarse índices de eficiencia de Nash-Sutcliffe cercanos a 0.9 en calibración y a 0.8 en validación, con parámetros dentro de los rangos establecidos en la literatura científica.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The calibration of a conceptual rainfall-runoff model is a complicated process that can take a long time and effort. Its success depends on the experience of the modeler and on the knowledge of the basin. For this reason, in this paper, a combination of manual and automatic calibration has been proposed to obtain the effective parameters of a hydrological model applied to a high mountain basin. This is because calibrating hydrological parameters and snow melting parameters simultaneously may not adequately represent the real conditions of high mountain systems. The methodology proposed in this paper has been implemented using the distributed hydrological TETIS model developed at the Universitat Politècnica de València. The results obtained are acceptable, because the Nash-Sutcliffe efficiency index is reached close to 0.9 in calibration and 0.8 validation, with parameters within the ranges established in the scientific literature.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Calibración]]></kwd>
<kwd lng="es"><![CDATA[algoritmo de optimización]]></kwd>
<kwd lng="es"><![CDATA[modelación hidrológica]]></kwd>
<kwd lng="es"><![CDATA[fusión de nieve]]></kwd>
<kwd lng="es"><![CDATA[método grado-día]]></kwd>
<kwd lng="en"><![CDATA[Calibration]]></kwd>
<kwd lng="en"><![CDATA[optimization Algorithm]]></kwd>
<kwd lng="en"><![CDATA[hydrological modeling]]></kwd>
<kwd lng="en"><![CDATA[snowmelt]]></kwd>
<kwd lng="en"><![CDATA[degree-day method]]></kwd>
</kwd-group>
</article-meta>
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