<?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>1405-3195</journal-id>
<journal-title><![CDATA[Agrociencia]]></journal-title>
<abbrev-journal-title><![CDATA[Agrociencia]]></abbrev-journal-title>
<issn>1405-3195</issn>
<publisher>
<publisher-name><![CDATA[Colegio de Postgraduados]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-31952017000600617</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[EFECTO DEL MESOCLIMA EN LA MADURACIÓN DE UVA NEBBIOLO (Vitis vinifera) EN EL VALLE DE GUADALUPE, BAJA CALIFORNIA, MÉXICO]]></article-title>
<article-title xml:lang="en"><![CDATA[THE EFFECT OF MESOCLIMATE ON THE RIPENING OF NEBBIOLO GRAPES (Vitis vinifera) IN VALLE DE VALLE DE GUADALUPE, BAJA CALIFORNIA, MEXICO]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cabello-Pasini]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Macias-Carranza]]></surname>
<given-names><![CDATA[Víctor]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mejía-Trejo]]></surname>
<given-names><![CDATA[Adán]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Baja California Instituto de Investigaciones Oceanológicas ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2017</year>
</pub-date>
<volume>51</volume>
<numero>6</numero>
<fpage>617</fpage>
<lpage>633</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-31952017000600617&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-31952017000600617&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-31952017000600617&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La fisiología de la vid (Vitis vinífera) está regulada por las condiciones climáticas de mesoescala y gran escala. El valle de Guadalupe es una cuenca vitivinícola que produce la mayoría del vino de México y presenta variaciones climáticas en mesoescala que podrían influenciar la maduración de las uvas. El objetivo de este estudio fue evaluar el efecto de las diferencias climáticas en dos zonas vitivinícolas del Valle de Guadalupe, sobre la maduración de la uva variedad Nebbiolo. Debido a la distancia con respecto a la costa, se esperaban encontrar diferencias climáticas en el valle y en la maduración de las uvas en las zonas de estudio. Durante cuatro temporadas, se evaluó concentración de sólidos solubles, acidez titulable y pH de uvas de la zona centro del Valle de Guadalupe y de la zona más cercana al mar, San Antonio de la Minas (SAM), Baja California, México. Además, se evaluó la temperatura, humedad relativa, irradiancia, precipitación pluvial, y velocidad y dirección del viento de 2012 al 2015. La concentración de sólidos solubles y el pH fueron significativamente mayores en el mosto de las uvas de Guadalupe que en las de SAM en las cuatro temporadas. Al contrario, la concentración de ácidos orgánicos fue siempre menor en el mosto de las uvas de Guadalupe que en las de SAM. La irradiancia fue similar en ambas zonas, pero la temperatura diaria promedio y el número de días con temperaturas extremas fueron mayores en Guadalupe. Al contrario, la humedad relativa y la precipitación fueron mayores en SAM. La maduración temprana de las uvas Nebbiolo de Guadalupe parece que es resultado de las temperaturas promedio mayores, los períodos frecuentes de calor y la humedad relativa menor en Guadalupe respecto a SAM.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The physiology of vines (Vitis vinifera) is regulated by the mesoscale and large-scale climatic conditions. Valle de Guadalupe is a winegrowing basin where most of Mexico&#8217;s wine production takes place and presents climatic variations in mesoscale that could influence the grape ripening. The objective of this study was to evaluate the effect of climatic differences on the ripening of the Nebbiolo grape variety, in two winegrowing areas of Valle de Guadalupe. Due to the distance from the coast, finding climatic differences in the valley and in the grape ripening in the study areas was to be expected. Over the course of four seasons, soluble solids concentration, titratable acidity, and pH were evaluated in grapes from the central zone of Valle de Guadalupe and the area nearest to the sea, San Antonio de la Minas (SAM), Baja California, Mexico. In addition, temperature, relative humidity, irradiance, rainfall, wind speed, and wind direction were evaluated from 2012 to 2015. The soluble solids concentration and pH were significantly higher in the Guadalupe grapes&#8217; must than in SAM grapes during the four seasons. On the contrary, the concentration of organic acids always was lower in the must of Guadalupe grapes than in the SAM&#8217;s. The irradiance was similar in both areas, but the daily average temperature and the number of days with extreme temperatures were higher in Guadalupe. On the contrary, relative humidity and precipitation were higher in SAM. The early ripening of Guadalupe&#8217;s Nebbiolo grapes seems to be the result of higher average temperatures, frequent warm periods, and lower relative humidity in Guadalupe compared with SAM.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[mesoclima]]></kwd>
<kwd lng="es"><![CDATA[temperatura]]></kwd>
<kwd lng="es"><![CDATA[Nebbiolo]]></kwd>
<kwd lng="es"><![CDATA[Valle de Guadalupe]]></kwd>
<kwd lng="es"><![CDATA[viticultura]]></kwd>
<kwd lng="es"><![CDATA[Vitis vinífera]]></kwd>
<kwd lng="en"><![CDATA[mesoclimate]]></kwd>
<kwd lng="en"><![CDATA[temperature]]></kwd>
<kwd lng="en"><![CDATA[Nebbiolo]]></kwd>
<kwd lng="en"><![CDATA[Valle de Guadalupe]]></kwd>
<kwd lng="en"><![CDATA[viticulture]]></kwd>
<kwd lng="en"><![CDATA[Vitis vinifera]]></kwd>
</kwd-group>
</article-meta>
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