<?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>0122-9761</journal-id>
<journal-title><![CDATA[Boletín de Investigaciones Marinas y Costeras - INVEMAR]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Invest. Mar. Cost.]]></abbrev-journal-title>
<issn>0122-9761</issn>
<publisher>
<publisher-name><![CDATA[INSTITUTO DE INVESTIGACIONES MARINAS Y COSTERAS "JOSE BENITO VIVES DE ANDRÉIS" (INVEMAR)    INSTITUTO DE INVESTIGACIONES MARINAS Y COSTERAS -JOSE BENITO VIVES DE ANDRÉIS- (INVEMAR)]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0122-97612021000300059</article-id>
<article-id pub-id-type="doi">10.25268/bimc.invemar.2021.50.suplesp.949</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Study of the Lange Glacier and its impact due to temperature increase in Admiralty Bay, King George Island, Antarctica]]></article-title>
<article-title xml:lang="es"><![CDATA[Estudio del glaciar Lange y su impacto debido al aumento de temperatura en la bahía Almirantazgo, isla Rey Jorge, Antártica]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mojica-Moncada]]></surname>
<given-names><![CDATA[Diego F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cárdenas]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mojica-Moncada]]></surname>
<given-names><![CDATA[Jhon F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Brondi]]></surname>
<given-names><![CDATA[Fabian]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barragán-Barrera]]></surname>
<given-names><![CDATA[Dalia C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Marangunic]]></surname>
<given-names><![CDATA[Cedomir]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Holland]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Franco Herrera]]></surname>
<given-names><![CDATA[Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Casassa]]></surname>
<given-names><![CDATA[Gino]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Magallanes  ]]></institution>
<addr-line><![CDATA[Punta Arenas ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Magallanes  ]]></institution>
<addr-line><![CDATA[Punta Arenas ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Programa Antártico Colombiano  ]]></institution>
<addr-line><![CDATA[Bogotá ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Instituto Geográfico Nacional del Perú  ]]></institution>
<addr-line><![CDATA[Lima ]]></addr-line>
<country>Perú</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Centro de Investigaciones Oceanográficas e Hidrográficas del Caribe-CIOH Dirección General Marítima ]]></institution>
<addr-line><![CDATA[Cartagena de Indias ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af6">
<institution><![CDATA[,Universidad de Magallanes Gaia Antarctica Research Center ]]></institution>
<addr-line><![CDATA[Punta Arenas ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af7">
<institution><![CDATA[,New York University Center for global Sea Level Change ]]></institution>
<addr-line><![CDATA[Abu Dhabi ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af8">
<institution><![CDATA[,Programa Antártico Colombiano  ]]></institution>
<addr-line><![CDATA[Bogotá ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af9">
<institution><![CDATA[,Universidad de Magallanes Gaia Antarctica Research Center ]]></institution>
<addr-line><![CDATA[Punta Arenas ]]></addr-line>
<country>Chile</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<volume>50</volume>
<fpage>59</fpage>
<lpage>84</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-97612021000300059&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-97612021000300059&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-97612021000300059&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In the western Antarctic Peninsula one of the areas the highest warming in the southern hemisphere has been identified. To characterize this tendency, we selected the Lange Glacier (LG) on King George Island, to evaluate: 1) LG surface temperature and dynamics using stakes with temperature data loggers; 2) LG submerged thickness and sea parameters through bathymetry (BT) and 29 CTD stations in front of LG; 3) glacier front (GF) using BT and a Digital Elevation Model (DEM); 4) change in GF position using DEM and historical data of GF width; 5) Calving flux (QC). Our findings showed 85 % of temperatures were above the 0 °C melting point (mean = 5.0 ± 5.2 °C). The stakes had an average ice loss of 9.3 ± 1.3 cm. The LG mean dynamics was 8.8 ± 1.5 m (0.40 ± 0.70 m/day), corroborated by Sentinel-1 satellite images (Offset Tracking = 0.43 ± 0.01 m/day). An intrusion of external waters warmer in the LG bay was identified, which destabilizes the water column due to convection processes. Our findings together indicated a continuous glacial melt that increases its dynamics due to the increase in temperature, with a contribution of fresh water to the Admiralty Bay. Based on historical results and this study, the LG retracement was estimated in 2,492 m between 1956 and 2019.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Al occidente de la Península Antártica se ha identificado una de las áreas de mayor calentamiento del hemisferio sur. Para caracterizar esta tendencia, se seleccionó el Glaciar Lange (GL) en la Isla Rey Jorge, con el fin de evaluar: 1) temperatura superficial y dinámica del GL utilizando estacas con sensores de temperatura; 2) espesor sumergido del GL y parámetros del mar a través de batimetría (BT) y 29 estaciones CTD frente al GL; 3) frente de glaciar (FG) utilizando BT y un Modelo Digital de Elevación (MDE); 4) cambio en la posición del FG usando MDE y datos históricos de su ancho; 5) flujo de Calving (QC). Los resultados mostraron que el 85 % de las temperaturas estuvieron por encima del punto de fusión de 0 °C (media = 5,0 ± 5,2 °C). Las estacas arrojaron una pérdida promedio de hielo de 9,3 ± 1,3 cm. La dinámica promedio del GL fue de 8,8 ± 1,5 m (0,40 ± 0,70 m/día), corroborado por imágenes de satélite Sentinel-1 (Offset Tracking = 0,43 ± 0,01 m/día). Se identificó una intrusión de aguas externas más cálidas que las aguas residentes en la bahía del GL, lo cual desestabiliza la columna de agua debido a procesos de convección. Nuestros hallazgos en conjunto indicaron una fusión glaciar continua que aumenta su dinámica debido al aumento de temperatura, con un aporte de agua dulce a la Bahía del Almirantazgo. Según los resultados históricos y este estudio, el retroceso del GL se estimó entre 1956 y 2019 en 2.492 m.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Lange Glacier]]></kwd>
<kwd lng="en"><![CDATA[Melting]]></kwd>
<kwd lng="en"><![CDATA[Climate change]]></kwd>
<kwd lng="en"><![CDATA[Calving flux]]></kwd>
<kwd lng="en"><![CDATA[Antarctica]]></kwd>
<kwd lng="es"><![CDATA[Glaciar Lange]]></kwd>
<kwd lng="es"><![CDATA[Deshielo]]></kwd>
<kwd lng="es"><![CDATA[Cambio Climático]]></kwd>
<kwd lng="es"><![CDATA[Flujo de Calving]]></kwd>
<kwd lng="es"><![CDATA[Antártica]]></kwd>
</kwd-group>
</article-meta>
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