<?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>S2007-09342017000801797</article-id>
<article-id pub-id-type="doi">10.29312/remexca.v8i8.703</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[El cambio climático afecta el número de horas de los rangos térmicos del chile en el norte-centro de México]]></article-title>
<article-title xml:lang="en"><![CDATA[Climate change affects the number of hours in the thermal ranges of chilli in North-Central Mexico]]></article-title>
</title-group>
<contrib-group>
<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[Mena-Covarrubias]]></surname>
<given-names><![CDATA[Jaime]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ruiz-Corral]]></surname>
<given-names><![CDATA[José Ariel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<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[Soria-Ruiz]]></surname>
<given-names><![CDATA[Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,INIFAP Campo Experimental Zacatecas ]]></institution>
<addr-line><![CDATA[Calera Zacatecas]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,INIFAP Campo Experimental Centro Altos de Jalisco ]]></institution>
<addr-line><![CDATA[Tepatitlán Jalisco]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,INIFAP Campo Experimental Pabellón ]]></institution>
<addr-line><![CDATA[Pabellón de Arteaga Aguascalientes]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,INIFAP Sitio Experimental Metepec ]]></institution>
<addr-line><![CDATA[Zinacantepec Estado de México]]></addr-line>
<country>Mexico</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>8</numero>
<fpage>1797</fpage>
<lpage>1812</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-09342017000801797&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-09342017000801797&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-09342017000801797&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En México el cultivo del chile tiene una larga tradición cultural y es uno de los principales centros de origen y domesticación, anualmente se siembran en promedio 97 306 ha en el Norte Centro del país. Sin embargo, la productividad del cultivo de chile es muy errática debido a factores bióticos y abióticos que se presentan durante su desarrollo. Temperaturas extremas y la disponibilidad de agua son dos de los factores de estrés abiótico dominantes. El objetivo de este trabajo fue conocer el efecto del calentamiento global, sobre el rango térmico del cultivo de chile. Se realizó un análisis histórico sobre la variación del número de horas con temperatura dentro y fuera del rango térmico de chile, y un análisis similar en los escenarios climáticos 2050 y 2070 en los RCP 4.5 y 8.5. Tanto en el análisis histórico como en las climatologías se encontraron efectos positivos y negativos del calentamiento global. El calentamiento global favorecerá al cultivo de chile con un aumento de la superficie (22.6%) con temperatura horaria dentro de los umbrales de desarrollo (15 a 32 °C) y un aumento de la superficie (15.8%) dentro del rango de temperatura óptima (18 a 28 °C). El cultivo de chile se verá limitado por el aumento (20.8%) de la superficie con temperatura horaria mayor al umbral superior (32 °C) y un aumento (18.5%) de la superficie con temperatura nocturna horaria mayor al umbral superior de temperatura nocturna (18 °C) en el RCP 4.5 y en la climatología 2050. El estrés por temperatura alta repercutirá en la disminución del rendimiento debido al efecto negativo en los procesos de polinización y amarre de frutos.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In Mexico, chili cultivation has a long cultural tradition and is one of the main centers of origin and domestication. An average of 97,306 ha is planted annually in the north of the country. However, the productivity of the chili crop is very erratic due to biotic and abiotic factors that occur during its development. Extreme temperatures and water availability are two of the dominant abiotic stressors. The objective of this work was to know the effect of global warming, on the thermal range of the chili crop. A historical analysis was performed on the variation of the number of hours with temperature inside and outside the thermal range of chili, and a similar analysis in the climatic scenarios 2050 and 2070 in the RCPs 4.5 and 8.5. Both in the historical analysis and in the climatologies we found positive and negative effects of global warming. Global warming will favor chilli cultivation with a surface increase (22.6%) with hourly temperature within development thresholds (15 to 32 °C) and a surface increase (15.8%) within the optimum temperature range (18 to 28 °C). Chili cultivation will be limited by the increase (20.8%) in the surface area with hourly temperature above the upper threshold (32 °C) and an increase (18.5%) in the area with a night time temperature above the upper threshold of night temperature (18 °C) in RCP 4.5 and in climatology 2050. High temperature stress will have an effect on the yield decrease due to the negative effect on pollination and fruit binding processes.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Capsicum annuum]]></kwd>
<kwd lng="es"><![CDATA[calentamiento global]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="es"><![CDATA[RCP]]></kwd>
<kwd lng="es"><![CDATA[temperatura horaria]]></kwd>
<kwd lng="en"><![CDATA[Capsicum annuum]]></kwd>
<kwd lng="en"><![CDATA[global warming]]></kwd>
<kwd lng="en"><![CDATA[hourly temperature]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="en"><![CDATA[RCP]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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