<?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>S0187-62362024000100048</article-id>
<article-id pub-id-type="doi">10.20937/atm.53380</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Chemical and isotopic composition of rainwater in the eastern Yucatan peninsula, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Camacho]]></surname>
<given-names><![CDATA[Daniela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Ríos]]></surname>
<given-names><![CDATA[Sofía]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Córdoba-Benavides]]></surname>
<given-names><![CDATA[Fernanda]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ladino]]></surname>
<given-names><![CDATA[Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cejudo]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro de Investigación Científica de Yucatán (CICY-CONAHCyT) Unidad de Ciencias del Agua ]]></institution>
<addr-line><![CDATA[Cancún Quintana Roo]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Ciencias de la Atmósfera y Cambio Climático ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>38</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362024000100048&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362024000100048&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362024000100048&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Given that rain is the component of precipitation that reaches the surface of the earth, and aiming to contribute to the global efforts of rainwater monitoring, we present information regarding the origin of ions and their relationship with isotopic patterns and the source of moisture for rainwater in the Mexican Caribbean, which not only may be useful for pollution and atmospheric studies, but also for estimating groundwater recharges, understanding dust nuisances, and offering information about water quality for rainwater harvesting. In this paper, we describe the chemical composition of rainwater in terms of major ions, isotopic composition, and the most probable sources of moisture in the Caribbean coastal zone of Mexico, considering the three main climatic seasons in this area. The chemistry of rainwater displayed a noticeable influence from sea-salt spray, land-blown dust, and anthropogenic impacts such as agriculture and biomass burning. We identified the predominant terrestrial origin of calcium, namely anthropogenic contributions of sulfates and nitrates, plus potassium from sea spray and anthropogenic emissions. The local meteoric water line is &#948;2H = 8.2 &#948;18O + 13.8 (R² = 0.9601) suggesting enrichment due to evaporative losses, various moisture sources and local climatic effects. Although isotope composition was not different by site, it was by season, as opposed to water chemistry. We conclude that the water chemistry responds to the local conditions of the air column below the clouds, while the isotope composition is influenced by the origin of moisture and the physical conditions in which water evaporates and condenses as well.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La lluvia es el componente de la precipitación que llega a la superficie terrestre. Con el fin de contribuir a los esfuerzos mundiales de monitoreo del agua de lluvia, presentamos información sobre la química del agua y su relación con la composición isotópica y la procedencia de la humedad que puede generar lluvia en el Caribe mexicano. Esta información es útil para estudios atmosféricos y de contaminación, así como para estimaciones de recarga de aguas subterráneas, problemas asociados con el polvo atmosférico y para proporcionar información para la recolección de agua de lluvia. En este artículo describimos la composición química del agua de lluvia (iones mayoritarios), su composición isotópica y las probables fuentes de humedad en la zona costera del Caribe mexicano, considerando las tres estaciones climáticas de esta zona. La química del agua mostró influencia de aerosoles marinos, polvo terrígeno e impactos antrópicos como la agricultura y la quema de biomasa. Identificamos el origen terrestre predominante del calcio, contribuciones antrópicas de sulfatos y nitratos, y potasio proveniente tanto del rocío marino como de emisiones antrópicas. La línea de agua meteórica local es &#948;2H = 8.2 &#948;18O + 13.8 (R² = 0.9601), lo que sugiere un enriquecimiento isotópico debido a pérdidas por evaporación, diferentes fuentes de humedad y efectos climáticos locales. La composición isotópica no fue diferente entre sitios, pero sí por estaciones climáticas, opuesto a la química del agua. Concluimos que la química del agua responde a las condiciones locales de la columna de aire bajo las nubes, mientras que la composición isotópica está influenciada por el origen de la humedad y las condiciones físicas en que el agua se evapora y condensa.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[backward air trajectories]]></kwd>
<kwd lng="en"><![CDATA[biomass burning]]></kwd>
<kwd lng="en"><![CDATA[isotopes]]></kwd>
<kwd lng="en"><![CDATA[sea-salt fraction]]></kwd>
<kwd lng="en"><![CDATA[soil dust]]></kwd>
</kwd-group>
</article-meta>
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