<?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>0187-6236</journal-id>
<journal-title><![CDATA[Atmósfera]]></journal-title>
<abbrev-journal-title><![CDATA[Atmósfera]]></abbrev-journal-title>
<issn>0187-6236</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Ciencias de la Atmósfera y Cambio Climático]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0187-62362023000100091</article-id>
<article-id pub-id-type="doi">10.20937/atm.53026</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Regional patterns of vegetation, temperature, and rainfall trends in the coastal mountain range of Chiapas, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Wootton]]></surname>
<given-names><![CDATA[Allen]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Enríquez]]></surname>
<given-names><![CDATA[Paula L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Navarrete-Gutiérrez]]></surname>
<given-names><![CDATA[Darío]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,El Colegio de la Frontera Sur Departamento de Conservación de la Biodiversidad ]]></institution>
<addr-line><![CDATA[San Cristóbal de las Casas Chiapas]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,El Colegio de la Frontera Sur Departamento de Observación y Estudio de la Tierra, la Atmósfera y el Océano ]]></institution>
<addr-line><![CDATA[San Cristóbal de las Casas Chiapas]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>36</volume>
<numero>1</numero>
<fpage>91</fpage>
<lpage>122</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362023000100091&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362023000100091&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362023000100091&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Changes in atmospheric CO2, ocean temperature, and regional vegetation conditions in Mesoamerica indicate that significant trends in temperature and rainfall may have occurred in the Sierra Madre de Chiapas, Mexico. This is an important region for flora and fauna which could be affected by climate trends. We aimed to determine if and where climate trends had occurred in the Sierra Madre and lower elevation regions between 1990 and 2016 (27 years), if these trends were part of longer term (1960-2016 [57 years]) changes, and how changes in large-scale and regional/local conditions may be influencing these trends. In the Sierra Madre, overall minimum daily temperatures increased, maximum temperatures decreased, and the most significant mean temperature trends were cooler during the 27-yr period. Both the start and end of the wet season trended earlier in the year, and wet season rainfall increased significantly. Trends were not significant during the 57-yr period in the Sierra Madre; however, in the adjacent Pacific coast region, significant warmer temperature trends continued during this period. Within regions, there was large variation in temperature and rainfall changes and some local trends were opposite to the regional averages. Large-scale processes of warming sea surface temperatures in the east coast of Mexico, a change from the positive to negative phase of the Pacific Decadal Oscillation and increases in atmospheric CO2 may be influencing these trends. At the regional scale, increases in dense vegetation and evapotranspiration since 1990 may have created characteristics favoring a positive feedback of higher ocean-based moisture and vegetation-based precipitation cycling.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los cambios en el CO2 atmosférico, la temperatura del océano y las condiciones de la vegetación regional en Mesoamérica indican posibles tendencias significativas en la temperatura y lluvias en la Sierra Madre de Chiapas, México. Ésta es una región importante para la flora la fauna que podría verse afectada por las tendencias climáticas. Nuestro objetivo fue determinar si se habían producido tendencias climáticas en un periodo de 27 años en la Sierra Madre y las regiones de menor elevación entre 1990 y 2016, si estas tendencias son parte de cambios a más largo plazo (1960-2016 [57 años]) y la manera en que los cambios en las condiciones de gran escala y regionales/locales pueden influir en estas tendencias. En la Sierra Madre, las temperaturas diarias mínimas generales aumentaron, las temperaturas máximas disminuyeron y la mayoría de las tendencias significativas de temperatura media fueron más frías durante el periodo de 27 años. Tanto el inicio como el final de la temporada húmeda mostraron una tendencia a principios de año, y las lluvias de esta temporada aumentaron significativamente. Las tendencias no fueron significativas durante el periodo de 57 años en la Sierra Madre; sin embargo, en la región adyacente de la costa del Pacífico, continuaron las tendencias significativas de temperaturas más cálidas durante este periodo. Hubo una gran variación en los cambios de temperatura y precipitación entre regiones, y algunas tendencias locales fueron opuestas a los promedios regionales. Es posible que los procesos a gran escala de calentamiento en las temperaturas de la superficie del mar en la costa este de México, un cambio de la fase positiva a negativa en la Oscilación Decenal del Pacífico y los aumentos en el CO2 atmosférico influyan en estas tendencias. A escala regional, los aumentos en la vegetación densa y la evapotranspiración desde 1990 pueden haber creado condiciones que favorezcan una retroalimentación positiva de mayor humedad oceánica y un ciclo de precipitación basado en la vegetación.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[climate trends]]></kwd>
<kwd lng="en"><![CDATA[evapotranspiration]]></kwd>
<kwd lng="en"><![CDATA[remote sensing]]></kwd>
<kwd lng="en"><![CDATA[Sierra Madre]]></kwd>
<kwd lng="en"><![CDATA[vegetation changes]]></kwd>
</kwd-group>
</article-meta>
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