<?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>S0187-62362017000400337</article-id>
<article-id pub-id-type="doi">10.20937/atm.2017.30.04.05</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Ozone climatology and variability over Irene, South Africa determined by ground based and satellite observations. Part 1: Vertical variations in the troposphere and stratosphere]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sivakumar]]></surname>
<given-names><![CDATA[Venkataraman]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ogunniyi]]></surname>
<given-names><![CDATA[Jeremiah]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,University of KwaZulu Natal School of Chemistry and Physics Discipline of Physics]]></institution>
<addr-line><![CDATA[Durban ]]></addr-line>
<country>South Africa</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<volume>30</volume>
<numero>4</numero>
<fpage>337</fpage>
<lpage>353</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362017000400337&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362017000400337&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362017000400337&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In this investigation, the climatological characteristics of ozone over Irene (25.5º S, 28.1º E) are studied with the aid of both ground-based and satellite observations. The principle aim of this work is therefore to examine the variability of vertical ozone distribution over Irene. Ozonesonde measurements and satellite measurements in the mesosphere-lower thermosphere region from the Microwave Limb Sounder (MLS) onboard the Aura satellite and it measures for the period 2004-2007 are employed in this study. The MLS satellite measurements are collected when it overpasses Irene. The vertical ozone profiles are obtained from ozonesondes and the MLS and are found to be in good agreement from a 15 km altitude and above. Maximum ozone concentration is found in the altitude between 23-27 km. The monthly variation of ozone concentration measured by ozonesondes and MLS show maximum and minimum concentrations during spring and autumn, respectively. During spring, the maximum ozone concentration measured by ozonesonde is 4.5 × 1012 molecules cm-3 while that measured by the MLS instrument is ~4.1 × 1012 molecules cm-3. A difference in the range of 0.4 × 1012 to 0.8 × 1012 molecules cm-3 was obtained for all seasons except during winter, when the difference was in the range 0.6 × 1012 to 0.9 × 1012 molecules cm-3.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[ Se estudian las características climatológicas del ozono sobre Irene, Sudáfrica (25.5º S, 28.1º E) con la ayuda de observaciones satelitales y de campo. El objetivo principal de este trabajo es, por lo tanto, analizar la variabilidad vertical de la distribución de ozono sobre Irene. Se utilizan mediciones de sonda de ozono y de la mesosfera-termosfera baja realizadas con la sonda para medición de microondas en la zona atmosférica limítrofe (Microwave Limb Sounder, MLS) del satélite Aura en el periodo 2004-2007. Las mediciones del MLS se recolectan cuando el instrumento pasa sobre Irene. Los perfiles verticales de ozono se obtienen mediante sondas de ozono y tienen buena concordancia con los obtenidos del MLS a una altitud de 15 km y superior. La mayor concentración de ozono se encuentra en la región comprendida entre los 23 y 27 km. La variación mensual de la concentración de ozono medida tanto por sondas como por el MLS muestra máximos y mínimos durante la primavera y el verano, respectivamente. En la primavera, las concentraciones de ozono medidas por sonda son de 4.5 × 1012 moléculas cm-3, en tanto que las medidas por el MLS son de ~4.1 × 1012 moléculas cm-3. Se encontró una diferencia en el rango de 0.4 × 1012 a 0.8 × 1012 moléculas cm-3 en todas las estaciones excepto en el invierno, cuando la diferencia fue de 0.6 × 1012 a 0.9 × 1012 moléculas cm-3.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Ozone]]></kwd>
<kwd lng="en"><![CDATA[vertical variations]]></kwd>
<kwd lng="en"><![CDATA[climatology]]></kwd>
<kwd lng="en"><![CDATA[South Africa]]></kwd>
</kwd-group>
</article-meta>
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