<?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>2007-4026</journal-id>
<journal-title><![CDATA[Ingeniería agrícola y biosistemas]]></journal-title>
<abbrev-journal-title><![CDATA[Ing. agric. biosist.]]></abbrev-journal-title>
<issn>2007-4026</issn>
<publisher>
<publisher-name><![CDATA[Universidad Autónoma Chapingo]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-40262017000100003</article-id>
<article-id pub-id-type="doi">10.5154/r.inagbi.2016.12.008</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Hydrological modeling of a basin in Mexico&#8217;s arid northern region and its response to environmental changes]]></article-title>
<article-title xml:lang="es"><![CDATA[Modelación hidrológica de una cuenca del norte árido de México y su respuesta a cambios ambientales]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Esquivel-Arriaga]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Nevarez-Favela]]></surname>
<given-names><![CDATA[María Magdalena]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Velásquez-Valle]]></surname>
<given-names><![CDATA[Miguel Agustín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Cohen]]></surname>
<given-names><![CDATA[Ignacio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bueno-Hurtado]]></surname>
<given-names><![CDATA[Palmira]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias  ]]></institution>
<addr-line><![CDATA[Gómez Palacio Durango]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma Chapingo  ]]></institution>
<addr-line><![CDATA[Bermejillo Durango]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias  ]]></institution>
<addr-line><![CDATA[Saltillo Coahuila]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2017</year>
</pub-date>
<volume>9</volume>
<numero>1</numero>
<fpage>3</fpage>
<lpage>18</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-40262017000100003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-40262017000100003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-40262017000100003&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract A basin&#8217;s hydrological services are becoming increasingly important due to the scarcity of water in many regions of the world. The aim of this research was to evaluate the impact of variations in climate patterns on runoff from the Sextín River basin using the Water Evaluation and Planning System (WEAP) hydrological model. The hydrological scheme was developed with vector and raster cartographic information, along with land-use, vegetation, climatological and hydrometric data of the study area. Model parameterization and calibration covered the period from 1971 to 2004. The model&#8217;s predictive performance was evaluated by NSE (Nash-Sutcliffe coefficient of efficiency), % BIAS and R2, obtaining values of 0.81, 12.1 and 0.81, respectively. Future regionalized climate change scenarios were generated with the Long Ashton Research Station Weather Generator (LARS-WG) on the basis of the Intergovernmental Panel on Climate Change (IPCC) A1B (rapid economic growth) and A2 (continuously increasing population) climate change scenarios, for the years 2020s (2010-2039) and 2050s (2040-2069). A possible mean annual increase of 1 °C, both for the maximum and minimum temperature, was observed in both analyzed periods. Increased precipitation and basin runoff were also projected in the regionalized climate scenarios. The information generated in this study can be useful for hydrological planning and management of the basin.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Dentro de los servicios de una cuenca se encuentran los hidrológicos, los cuales cada vez cobran más importancia debido a la escasez de agua en muchas regiones del mundo. El objetivo de esta investigación fue evaluar el impacto de las variaciones de los patrones climáticos sobre el escurrimiento de la cuenca del río Sextín mediante el modelo hidrológico Water Evaluation and Planning System (WEAP). El esquema hidrológico se elaboró con información cartográfica de tipo vectorial y raster, datos de uso de suelo, vegetación, climatológicos e hidrométricos de la zona de estudio. La parametrización y calibración del modelo comprendió de 1971 a 2004. La eficiencia predictiva del modelo se evaluó mediante NSE (Coeficiente de eficiencia de Nash-Sutcliffe), % BIAS y R2, obteniéndose valores de 0.81, 12.1 y 0.81, respectivamente. Se generaron escenarios regionalizados futuros de cambio climático con el modelo Long Ashton Research Station Weather Generator (LARS-WG), correspondientes a Intergovernmental Panel on Climate Change (IPCC): A1B (crecimiento económico rápido) y A2 (incremento continuo de la población), para los años 2020s (2010-2039) y 2050s (2040-2069). Se observó un posible incremento promedio anual de 1 °C, tanto para la temperatura máxima como mínima, en ambos periodos analizados. Referente a la precipitación, se proyectó un aumento, al igual que en el escurrimiento de la cuenca en los escenarios climáticos regionalizados. La información generada en este estudio puede ser de utilidad para ordenación y gestión hidrológica de la cuenca.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[runoff]]></kwd>
<kwd lng="en"><![CDATA[climate change]]></kwd>
<kwd lng="en"><![CDATA[management]]></kwd>
<kwd lng="en"><![CDATA[cartographic information.]]></kwd>
<kwd lng="es"><![CDATA[escurrimiento]]></kwd>
<kwd lng="es"><![CDATA[cambio climático]]></kwd>
<kwd lng="es"><![CDATA[gestión]]></kwd>
<kwd lng="es"><![CDATA[información cartográfica]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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