<?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>S0187-62362025000100022</article-id>
<article-id pub-id-type="doi">10.20937/atm.53423</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Influence of ENSO and SAM on the occurrence of absolute extremes and behavior of Ta, SST, and SIC anomalies in the western Antarctic Peninsula]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Montaño Bello]]></surname>
<given-names><![CDATA[Daniela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Villegas Bolaños]]></surname>
<given-names><![CDATA[Nancy Liliana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional de Colombia Departamento de Geociencias ]]></institution>
<addr-line><![CDATA[Bogotá D.C. ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional de Colombia Departamento de Geociencias ]]></institution>
<addr-line><![CDATA[Bogotá D.C. ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<volume>39</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362025000100022&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362025000100022&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362025000100022&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This study aims to improve the understanding of the interaction between El Niño-Southern Oscillation (ENSO) events and the phases of the Southern Annular Mode (SAM), as well as their influence on the western Antarctic Peninsula (WAP). Monthly series of air temperature (Ta), sea surface temperature (SST), and sea ice coverage (SIC) from 1981 to 2020 were analyzed at six representative points within the study area. Ta, SIC, and SST data were obtained from the ERA5 database. The Southern Oscillation Index (SOI) and Antarctic Oscillation Index (AAOI) were sourced from NOAA&#8217;s Climate Prediction Center. The spectral density of the anomaly series for each variable was calculated, and the characteristic cycles of SAM and ENSO were extracted. The most influential components driving the oscillations of the studied series were identified. A cross-correlation analysis was conducted between the anomaly components of Ta, SIC, and SST and those of SOI and AAOI. The results indicate that Ta series exhibit moderate positive correlations with SAM, particularly between the 5.2-year quasi-period of AAOI and the 4.4-year quasi period of Ta in the Drake Passage and Bransfield Strait. The SST series in Bransfield correlate with AAOI5.2, while the quasi-periods of 4.6 and 5.2 years in the Drake Passage correlate with SOI3.5. The SIC series show positive correlations with the 3.5-year quasi-period of SOI for lag times greater than one year, except in the Bransfield Strait. Extreme absolute Ta and SST events in the WAP region are strongly influenced by SAM and ENSO. It is concluded that the coupling of ENSO and SAM phases amplifies their effects on meteo-marine variables.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El objetivo de este trabajo es mejorar la comprensión de la interacción entre los eventos de El Niño-Oscilación del Sur (ENOS) y las fases de la Oscilación Antártica (OAA), así como su influencia en el oeste de la Península Antártica (OPA). Se utilizaron series mensuales de temperatura del aire (Ta), temperatura superficial del mar (TSM) y cobertura de hielo marino (CHM) del periodo 1981-2020 para seis puntos representativos de la región de estudio. Los datos de Ta, CHM y TSM fueron obtenidos de la base de datos ERA5. Los índices de la Oscilación del Sur (IOS) y la Oscilación Antártica (IOAA) fueron extraídos del Centro de Predicción del Clima de la NOAA. Se realizó el cálculo de la densidad espectral de las series de anomalías de cada variable y su descomposición en ciclos característicos de la OAA y el ENOS. Se identificaron los componentes más influyentes en las oscilaciones de las series de estudio. Se llevó a cabo un análisis de correlación cruzada entre las componentes de las anomalías de Ta, CHM y TSM, y los índices IOS y IOAA. Se encontró que las series de Ta presentan correlaciones positivas y moderadas con la OAA, particularmente entre el cuasiperiodo de 5.2 años del IOAA y el cuasiperiodo de 4.4 años de Ta para el Paso de Drake y el Estrecho de Bransfield. Las series de TSM en Bransfield se correlacionan con el IOAA5.2, mientras que los cuasiperiodos de 4.6 y 5.2 años en el Paso de Drake se correlacionan con el IOS3.5. Las series de CHM muestran correlaciones positivas con el cuasiperíodo de 3.5 años del IOS cuando los rezagos son superiores a un año, excepto en el Estrecho de Bransfield. Los eventos extremos de Ta y TSM en la región OPA están fuertemente influenciados por la OAA y el ENOS. Se concluye que el acoplamiento de las fases del ENOS y la OAA amplifica los efectos sobre las variables meteo-marinas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[ERA5]]></kwd>
<kwd lng="en"><![CDATA[correlation]]></kwd>
<kwd lng="en"><![CDATA[spectral density]]></kwd>
<kwd lng="en"><![CDATA[Bransfield]]></kwd>
<kwd lng="en"><![CDATA[Gerlache]]></kwd>
</kwd-group>
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