<?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>S0187-62362019000100055</article-id>
<article-id pub-id-type="doi">10.20937/atm.2019.32.01.05</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Spatial and temporal variation of acid rain in the Mexico City Metropolitan Zone]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sosa-Echeverría]]></surname>
<given-names><![CDATA[Rodolfo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alarcón-Jimémez]]></surname>
<given-names><![CDATA[Ana Luisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Torres-Barrera]]></surname>
<given-names><![CDATA[María del Carmen]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jaimes-Palomera]]></surname>
<given-names><![CDATA[Mónica]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Retama-Hernández]]></surname>
<given-names><![CDATA[Armando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Álvarez]]></surname>
<given-names><![CDATA[Pablo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Granados Hernández]]></surname>
<given-names><![CDATA[Elías]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bravo-Álvarez]]></surname>
<given-names><![CDATA[Humberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Ciencias de la Atmósfera ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Gobierno de la Ciudad de México Secretaría del Medio Ambiente ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>México</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Centro Tecnológico Aragón Facultad de Estudios Superiores Aragón ]]></institution>
<addr-line><![CDATA[Estado de México ]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>32</volume>
<numero>1</numero>
<fpage>55</fpage>
<lpage>69</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362019000100055&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362019000100055&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362019000100055&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT At the end of the 1980´s particulates and sulfur dioxide (SO2) were the main atmospheric pollutants in the Mexico City Metropolitan Zone (MCMZ). To reduce emissions, fuel oil was replaced by natural gas at power plants located inside Mexico City. Currently, SO2 levels do not exceed its air quality standard; however, acid rain is present with a high contribution of sulfate (SO4 2-). In this study, spatial and temporal variations in the chemical composition of rain in Mexico City between 2003 and 2014 were analyzed. Major ions (Na+, NH4 +, K+, Mg2+, Ca2+, SO4 2-, NO3 - and Cl-), pH, and electrical conductivity (EC) were analyzed weekly at 16 sampling stations located in the MCMZ. The pH decreased from north to south, with the lowest annual volume weighted mean (VWM) of 4.16 in 2006. Annual ion concentrations were, in decreasing order: NH4 +, SO4 2-, NO3 - and Ca2+ for the entire study period at most of the sampling sites. The highest values for wet atmospheric deposition (kg/ha) were found in the Western area and were the maximum in 2007. Wet deposition had major levels for SO4 2- and NO3 - of 24 and 20 kg/ha, respectively, and were similar to the levels registered in the USA in 2013 and 2014. Considering that external emission sources play a decisive role in acid rain within the City, it is necessary to establish strategies for the emission reductions of acid rain precursors from upwind sources.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN A finales de la década de 1980, las partículas y el bióxido de azufre (SO2) fueron los principales contaminantes atmosféricos en la Zona Metropolitana de la Ciudad de México (ZMCM). Para reducir esta problemática, el combustóleo fue sustituido por gas natural en las centrales termoeléctricas localizadas dentro de la Ciudad de México. Actualmente, los niveles de SO2 no exceden la norma de calidad del aire para este gas; sin embargo, se presenta lluvia ácida con una alta contribución de sulfatos (SO4 2-). En este estudio, se analizó la variación espacial y temporal de la composición química de la lluvia en la Ciudad de México de 2003 a 2014. Se colectaron muestras semanales en las que se analizaron los iones principales (Na+, NH4 +, K+, Mg2+, Ca2+, SO4 2-, NO3 - y Cl-), pH y conductividad eléctrica (CE) en 16 estaciones de muestreo ubicadas en la ZMCM. El pH disminuyó de norte a sur, con el valor anual más bajo del promedio ponderado por volumen (PPV) de 4.16 en 2006. Las concentraciones ponderadas anuales de los iones fueron, en orden decreciente: NH4 +, SO4 2-, NO3 - y Ca2+ durante todo el periodo de estudio en casi todos los sitios de muestreo. Los valores máximos de depósito atmosférico húmedo (kg/ha) se encontraron en el área oeste de la zona de estudio, siendo los más altos los registrados en 2007. Los mayores niveles de depósito húmedo encontrados fueron de 24 y 20 kg ha-1 para SO4 2- y NO3 -, respectivamente, y fueron similares a los niveles registrados en EUA en 2013 y 2014. Considerando que las fuentes de emisión externas juegan un papel decisivo en la lluvia ácida dentro de la Ciudad de México, es necesario establecer estrategias para la reducción de emisiones de precursores de lluvia ácida en las fuentes localizadas viento arriba.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Mexico City Metropolitan Zone]]></kwd>
<kwd lng="en"><![CDATA[wet deposition]]></kwd>
<kwd lng="en"><![CDATA[acid rain]]></kwd>
<kwd lng="en"><![CDATA[rain chemical composition]]></kwd>
<kwd lng="en"><![CDATA[acid rain precursors]]></kwd>
</kwd-group>
</article-meta>
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