<?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>2007-2422</journal-id>
<journal-title><![CDATA[Tecnología y ciencias del agua]]></journal-title>
<abbrev-journal-title><![CDATA[Tecnol. cienc. agua]]></abbrev-journal-title>
<issn>2007-2422</issn>
<publisher>
<publisher-name><![CDATA[Instituto Mexicano de Tecnología del Agua, Coordinación de Comunicación, Participación e Información]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-24222017000600023</article-id>
<article-id pub-id-type="doi">10.24850/j-tyca-2017-06-02</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Annual and monthly runoff analysis in the Elqui River, Chile, a semi-arid snow-glacier fed basin]]></article-title>
<article-title xml:lang="es"><![CDATA[Análisis de la escorrentía anual y mensual en el río Elqui, Chile, una cuenca semi árida de régimen nivoglaciar]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Balocchi]]></surname>
<given-names><![CDATA[Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
<xref ref-type="aff" rid="A a"/>
<xref ref-type="aff" rid="A3"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pizarro]]></surname>
<given-names><![CDATA[Roberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Meixner]]></surname>
<given-names><![CDATA[Thomas]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Urbina]]></surname>
<given-names><![CDATA[Fernando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,University of Arizona Department of Hydrology and Water Resources ]]></institution>
<addr-line><![CDATA[Tucson AZ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Forestal  ]]></institution>
<addr-line><![CDATA[Santiago ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Talca Centro Tecnológico de Hidrología Ambiental ]]></institution>
<addr-line><![CDATA[Talca ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Dirección General de Aguas Unidad de Hidrología ]]></institution>
<addr-line><![CDATA[Iquique ]]></addr-line>
<country>Chile</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2017</year>
</pub-date>
<volume>8</volume>
<numero>6</numero>
<fpage>23</fpage>
<lpage>35</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-24222017000600023&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-24222017000600023&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-24222017000600023&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Climate change and its relationship to temperature are critical factors affecting glaciers, especially when populations depend on these ice reservoirs. The use of the precipitation-runoff coefficient in semi-arid, mountainous regions that are fed by glaciers can lead to important findings about how glacial melt responds to climate change. This study analyzed 40 years of monthly and annual precipitation and runoff data (1970-2009) from four sub-basins of the Elqui River (29° 27&#8217;- 30° 34&#8217; S and 71° 22&#8217;- 69° 52&#8217; W), in the Coquimbo region of Chile. The Elqui basin has a rain-snow-glacial melt regime. The areal average rainfall was estimated using the Thiessen polygon method. Gumbel and Goodrich probability distribution functions and the Log-Normal Probability Density Function (PDF) were used to understand the temporal behavior of precipitation and streamflow. The data-time behavior and PP Q-1 coefficients were also analyzed. And the Mann-Kendall (MK) test was used to compare the results. No trends were found for flow, while a negative trend in rainfall was identified. The summer flows were notable, which remained constant. In spite of the differences between the PP Q-1 coefficient and the MK test, the flow clearly does not come from rainfall but rather from glacial melt.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: El cambio climático y su relación con la temperatura es un factor crítico que afecta a los glaciares, especialmente cuando la población depende de las reservas de hielo. Usando la relación precipitación-escorrentía en regiones montañosas semiáridas alimentadas por glaciares se pueden llevar a cabo importantes descubrimientos sobre cómo el derretimiento glaciar responde al cambio climático. En este estudio se analizaron 40 años (1970-2009) de datos de precipitación y escorrentía mensual y anual en cuatro subcuencas del río Elqui (29° 27&#8217;- 30° 34&#8217; S y 71° 22&#8217;- 69° 52&#8217; O) en la región de Coquimbo, Chile. La cuenca del Elqui posee un régimen pluvionivoglaciar. La precipitación areal promedio se estimó usando el método de polígonos de Thiessen. Se utilizaron las funciones de distribución de probabilidad de Gumbel, Goodrich y Log-Normal, con el fin de entender el comportamiento temporal de ambas variables. También se analizaron la variación temporal y el coeficiente PP Q-1. El test Mann-Kendall (MK) se empleó para comparar los resultados; no se encontraron tendencias para el caudal, pero sí una tendencia negativa en las precipitaciones. Vale la pena destacar los caudales de verano, los cuales se mantuvieron constantes. A pesar de las diferencias entre el coeficiente PP Q-1 y el test de MK, es claro que el caudal no proviene de las precipitaciones sino del fenómeno de derretimiento nivoglaciar.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Glacial melt]]></kwd>
<kwd lng="en"><![CDATA[Mann-Kendall]]></kwd>
<kwd lng="en"><![CDATA[precipitation and flow coefficient]]></kwd>
<kwd lng="en"><![CDATA[glacier-fed basin]]></kwd>
<kwd lng="en"><![CDATA[Gumbel distribution]]></kwd>
<kwd lng="en"><![CDATA[rainfall and flow trend]]></kwd>
<kwd lng="es"><![CDATA[derretimiento glacial]]></kwd>
<kwd lng="es"><![CDATA[Mann-Kendall]]></kwd>
<kwd lng="es"><![CDATA[coeficiente precipitación-caudal]]></kwd>
<kwd lng="es"><![CDATA[cuenca glaciar]]></kwd>
<kwd lng="es"><![CDATA[distribución de Gumbel]]></kwd>
<kwd lng="es"><![CDATA[tendencias de precipitación y caudal]]></kwd>
</kwd-group>
</article-meta>
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