<?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>0188-8897</journal-id>
<journal-title><![CDATA[Hidrobiológica]]></journal-title>
<abbrev-journal-title><![CDATA[Hidrobiológica]]></abbrev-journal-title>
<issn>0188-8897</issn>
<publisher>
<publisher-name><![CDATA[Universidad Autónoma Metropolitana, División de Ciencias Biológicas y de la Salud]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0188-88972017000100013</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Respuesta hidrológica al cambio climático en regiones áridas: caso de estudio en los Comondú, Baja California Sur, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Hydrologic response to climate change in arid regions: Case study in los Comondú, Baja California Sur, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wurl]]></surname>
<given-names><![CDATA[Jobst]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-García]]></surname>
<given-names><![CDATA[Cynthia Nayeli]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Imaz-Lamadrid]]></surname>
<given-names><![CDATA[Miguel Ángel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Baja California Sur de Conocimiento de Ciencias del Mar y de la Tierra Laboratorio de Hidrogeología]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Petróleos Mexicanos  ]]></institution>
<addr-line><![CDATA[Villahermosa Tabasco]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>04</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>04</month>
<year>2017</year>
</pub-date>
<volume>27</volume>
<numero>1</numero>
<fpage>13</fpage>
<lpage>22</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0188-88972017000100013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0188-88972017000100013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0188-88972017000100013&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen  Antecedentes: En la actualidad, el cambio climático es uno de los fenómenos con mayor relevancia dentro del medio científico; dicho proceso se ha registrado como un incremento de las temperaturas a escala global. Para la zona central de Baja California Sur (BCS), México, los modelos climáticos indican, además, un aumento en la frecuencia de precipita ciones extremas. El área de estudio abarca dos poblaciones (San José y San Miguel de Comondú) cuyas zonas urbanas y rurales se encuentran ubicadas en una cañada de aproximadamente 16 km de longitud y hasta 800 m de ancho.  Objetivos: Realizar un análisis estadístico histórico de la variabilidad climática y modelar la respuesta del arroyo Comondú ante eventos extremos de precipitación.  Métodos: Se analizó la variabilidad climática de acuerdo con las bases de datos de la estación climatológica de Comondú, operada por el Servicio Meteorológico Nacional (SMN). También se determinó el patrón de los escurrimientos en el arroyo Comondú durante episodios de precipitación extrema, similares o cercanos a eventos con tiempo de retorno de 1000 años por medio de los modelos hidrológicos e hidráulicos de los software HEC-1 y HEC-RAS.  Resultados: Para el caso de los Comondú, se observa una clara tendencia a la alza en los datos de preci pitación extrema de 24 horas, lo cual implica que el peligro de inundaciones en la zonas pobladas y de cultivos aumenta considerablemente. La ocurrencia de un evento de 1000 años afectaría cerca de 86,864 m2 en la zona urbana de ambos poblados y 201,570 m2 en la zona de cultivo.  Conclusiones: Los resultados de la modelación indican un incremento en área, profundidad y velocidad de la corriente, lo que aumenta el riesgo de inundación en las zonas bajas de los Comondú. Con base en los resultados de la modelación, se pueden promover medidas que permitan salvaguardar a la población y la economía de este lugar.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract  Background: Currently, climate change is one of the most relevant phenomena within the scientific environment; this change has been recorded as an increase in temperatures on a global scale. For the central zone of Baja California Sur (BCS), Mexico, climate models also indicate an increase in the frequency of extreme precipitation. The study area covers two towns (San José and San Miguel de Comondú) whose urban and rural areas are located in a ravine of approximately 16 km in length and up to 800 m in width.  Goals: To carry out a historical, statistical analysis of the climatic variability and model the response of the Comondú stream to extreme precipitation events.  Methods: Climatic variability was analyzed with databases from the Comondú weather station, operated by the National Meteorological Service (SMN). In addition, the runoff pattern in the Comondú stream was ascertained in the event of extreme precipitation events, similar to or close to events with a return time of 1000 years, using hydrological and hydraulic models of HEC-1 and HEC-RAS software.  Results: In the case of Los Comondú, BCS, there is a clear upward trend in the 24-hour extreme precipitation data, which implies that the danger of flooding in populated areas and crops increases considerably. The occurrence of a 1000-year event would affect about 86,864 m2 of the urban area of &#8203;&#8203;both towns and 201,570 m2 of the area under cultivation.  Conclusions: The results of our modeling indicate an increase in area, depth, and speed of the stream, increasing the risk of flooding in the lower areas of Los Comondú, BCS. Based on our modeling&#8217;s results, measures should be promoted to safeguard the population and the economy of Los Comondú.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Análisis de precipitaciones]]></kwd>
<kwd lng="es"><![CDATA[cambio climático]]></kwd>
<kwd lng="es"><![CDATA[inundaciones]]></kwd>
<kwd lng="es"><![CDATA[modelación hidráulica]]></kwd>
<kwd lng="en"><![CDATA[Climate change]]></kwd>
<kwd lng="en"><![CDATA[floods]]></kwd>
<kwd lng="en"><![CDATA[hydraulic modeling]]></kwd>
<kwd lng="en"><![CDATA[rainfall analysis]]></kwd>
</kwd-group>
</article-meta>
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