<?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>2007-0934</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias agrícolas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Mex. Cienc. Agríc]]></abbrev-journal-title>
<issn>2007-0934</issn>
<publisher>
<publisher-name><![CDATA[Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-09342014001401923</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Efecto de la condición ENSO en la frecuencia e intensidad de los eventos de lluvia en la península de Baja California (1998-2012)]]></article-title>
<article-title xml:lang="en"><![CDATA[Effect of the ENSO condition in the frequency and intensity of rainfall events in the Baja California peninsula (1998-2012)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez-Moreno]]></surname>
<given-names><![CDATA[Víctor Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ruíz-Corral]]></surname>
<given-names><![CDATA[José Ariel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Medina-García]]></surname>
<given-names><![CDATA[Guillermo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Padilla-Ramírez]]></surname>
<given-names><![CDATA[José Saúl]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gunter Kretzschmar]]></surname>
<given-names><![CDATA[Thomas]]></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 Campo Experimental Pabellón ]]></institution>
<addr-line><![CDATA[Pabellón de Arteaga Aguascalientes]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias Campo Experimental Altos de Jalisco ]]></institution>
<addr-line><![CDATA[Tepatitlán de Morelos Jalisco]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias  ]]></institution>
<addr-line><![CDATA[Calera de Victor Rosales Zacatecas]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE)  ]]></institution>
<addr-line><![CDATA[Ensenada B.C.]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2014</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2014</year>
</pub-date>
<volume>5</volume>
<numero>spe10</numero>
<fpage>1923</fpage>
<lpage>1937</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-09342014001401923&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-09342014001401923&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-09342014001401923&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: La influencia de la condición ENSO en la frecuencia e intensidad de los eventos de lluvia en la provincia fisiográfica Península de Baja California, se analizó conforme una serie histórica de 15 años de registros diarios de lluvia TRMM. La base de datos fue estratificada en siete categorías a intervalos de 5 mm; se consideraron los eventos extremos como &gt;30 mm día-1. Se obtuvieron indicios de que la condición ENSO influye en la frecuencia e intensidad de los eventos de lluvia. Se observó una cierta simetría entre las condiciones ENSO-Neutro y ENSO-La Niña Débil, y ENSO-El Niño Débil con ENSO-La Niña Moderada, que ocasionan un aumento en la frecuencia de los eventos de lluvia y una disminución en los mismos, respectivamente. En cuanto a la intensidad de la lluvia, otras relaciones simétricas fueron entre la condición ENSO-Neutro y ENSO-El Niño Débil y asimétricas entre las condiciones ENSO-La Niña Moderada y ENSO-La Niña Fuerte. La intensidad de las lluvias fue mayor durante las condiciones Neutro y El Niño Débil y menor durante las condiciones La Niña Moderada y La Niña Fuerte. Estos resultados son importantes debido a que los cambios en la frecuencia e intensidad de los eventos extremos son la consecuencia más dramática de la variabilidad climática y que afectan directamente la funcionalidad de los ecosistemas, su conformación paisajística y las fronteras espaciales del uso del suelo. La relación entre la frecuencia de ocurrencia y la intensidad de los eventos extremos, la condición ENSO y la presencia de huracanes está aún bajo investigación.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: The influence ofthe ENSO condition in the frequency and intensity of rainfall events in the physiographic province Baja California Peninsula was analysed as a historical series of 15 years of daily rainfall records TRMM. The database was stratified into seven categories at intervals of 5 mm; the extreme events considered as &gt; 30 mm day-1. We gathered evidence that, the ENSO condition influences the frequency and intensity of rainfall events. We also observed a certain symmetry between the conditions ENSO-neutral and ENSO-week La Niña and ENSO-weak El Niño with ENSO-moderate La Niña, causing an increase in the frequency ofrain events and a decrease, respectively. Regarding the intensity of the rain, other symmetrical relations were between the condition ENSO-neutral and ENSO-weak El Niño and asymmetrical between the conditions ENSO-moderate La Niña and ENSO-Strong La Niña. The rainfall intensity was higher during the conditions Neutral and Weak El Niño and lower during the conditions Moderate La Niña and Strong La Niña. These results are important because changes in the frequency and intensity of extreme events are the most dramatic consequence of climate variability, directly affecting the functioning of ecosystems, their landscape formation and spatial boundaries ofthe land use. The relationship between the frequency of occurrence and intensity of extreme events, the ENSO condition and the presence ofhurricanes is still under investigation.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[ENSO]]></kwd>
<kwd lng="es"><![CDATA[eventos extremos]]></kwd>
<kwd lng="es"><![CDATA[provincia fisiográfica]]></kwd>
<kwd lng="es"><![CDATA[TRMM]]></kwd>
<kwd lng="en"><![CDATA[ENSO]]></kwd>
<kwd lng="en"><![CDATA[extreme events]]></kwd>
<kwd lng="en"><![CDATA[physiographic province,TRMM]]></kwd>
</kwd-group>
</article-meta>
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