<?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>0188-4611</journal-id>
<journal-title><![CDATA[Investigaciones geográficas]]></journal-title>
<abbrev-journal-title><![CDATA[Invest. Geog]]></abbrev-journal-title>
<issn>0188-4611</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geografía]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0188-46112020000300005</article-id>
<article-id pub-id-type="doi">10.14350/rig.60153</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The effects of climatic change on glacial, proglacial and paraglacial systems at Collins Glacier, King George Island, Antarctica, from the end of the Little Ice Age to the 21st century]]></article-title>
<article-title xml:lang="es"><![CDATA[Los efectos de los cambios climáticos en los sistemas glaciales, proglaciales y periglaciales del glaciar Collins, isla Rey Jorge, Antártica, del final de la Pequeña Edad del Hielo al siglo XXI]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Petsch]]></surname>
<given-names><![CDATA[Carina]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rosa]]></surname>
<given-names><![CDATA[Kátia Kellem da]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vieira]]></surname>
<given-names><![CDATA[Rosemary]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Braun]]></surname>
<given-names><![CDATA[Matthias Holger]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Costa]]></surname>
<given-names><![CDATA[Rafaela Mattos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Simões]]></surname>
<given-names><![CDATA[Jefferson Cardia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Federal University of Santa Maria Department of Geosciences ]]></institution>
<addr-line><![CDATA[Santa Maria ]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Federal University of Rio Grande do Sul Polar and Climatic Center Geosciences Institute]]></institution>
<addr-line><![CDATA[Porto Alegre ]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Federal Fluminense University Geosciences Institute Laboratory of Sedimentary and Environmental Processes]]></institution>
<addr-line><![CDATA[Niterói Rio de Janeiro]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Friedrich-Alexander-Universität Institute of Geography ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Germany</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Federal University of Rio Grande do Sul Polar and Climatic Center Geosciences Institute]]></institution>
<addr-line><![CDATA[Porto Alegre ]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af6">
<institution><![CDATA[,University of Rio Grande do Sul Polar and Climatic Center Geosciences Institute]]></institution>
<addr-line><![CDATA[Porto Alegre ]]></addr-line>
<country>Brazil</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<numero>103</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0188-46112020000300005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0188-46112020000300005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0188-46112020000300005&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The analysis of glacial and ice-marginal systems may contribute to understanding the impact of climatic change. The aim of this study is to investigate changes in the glacial, proglacial and paraglacial system in response to the Collins glacier retreat, between the Little Ice Age (LIA) and 2070. Glacial geomorphological mapping reveals landforms that are diagnostic of a terrestrial-terminating glacier in the past. Glacial and the proglacial systems were mapped to evaluate the ice-marginal evolution. The field measurement, satellite imagery, granulometric and morphoscopic sedimentary analysis, and geomorphological data are analyzed. The Collins glacier surface topography has been surveyed by DGNSS during 11 years (1997/98-2008/09) and for glacier area estimation in 2030, 2050 and 2070 CE. The Collins glacier lost 1.4 km² in the period LIA-2018. Under an atmospheric warming scenario, using the temperature melt index model the glacier will lose approximately 5% of its total area until 2030 (0.90 km²), 21% (3.60 km²) by 2050, and 35% (5.90 km²) by 2070 CE. Four sectors in the proglacial zone are identified: Sector 1 displays changes on the front of the glacier since the LIA, a push moraine in only one sector, presence of flutings and moraines of recession. Sector 2 showed shrinkage around 100 meters in the period LIA-2018, presenting recessional and push moraines of about 10 meters of height. Sector 3 showed 350 meters of the shrinkage since the LIA, and recessional moraines, and absence of the push moraines. Sector 4, showed 1500 meters of the shrinkage since the LIA, a push moraine of about 12 meters high. This behavior that occurs since the LIA allows validating the future scenario model. The ice-free areas could expand 1,4 km² by the end of 2070 decade if considered since LIA. However, it should be noted that if the glacier continues to retreat, the system will be subject to hydrological and sedimentary readjustments at various stages in the future.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El análisis de los sistemas glaciales y marginales al hielo puede contribuir para la comprensión del impacto de los cambios climáticos. De esta forma, el objetivo de este estudio es investigar los cambios en el sistema glacial, proglacial y periglacial en respuesta al retroceso del glaciar Collins, entre la Pequeña Edad del Hielo (PEH) y 2070. La Península Fildes, parte sur de la isla Rey Jorge (latitud entre 62° 08' y 62° 14' S y longitud entre 59°02' e 58°51' O), es una de las primeras áreas a quedarse libre del hielo en el archipiélago de las Shetland del Sur después del Último Máximo Glacial. La elección por esta área de estudio en la isla Rey Jorge se justifica por la facilidad de se accender a ella para la realización de trabajos de campo y también porque hay investigaciones previas sobre ella que indican la retracción de los glaciales. Para evaluar la evolución marginal del hielo se mapearon los sistemas glacial y proglacial. Se interpretaron y se delimitaron las etapas de retracción desde la PEH por la posición de las morrenas de recesión y por la cronología establecida por imágenes de satélite. Se utilizaron imágenes Landsat de los sensores TM, ETM+ y OLI referentes a las fechas 03/01/1986, 27/02/1988, 28/01/1989, 19/01/2003, 17/03/2015 y 29/04/2018 para establecer los valores de retracción del glaciar Collins. Para elaborar el mapeo geomorfológico actual se analizaron datos de trabajos de campo realizados en 2013, 2014 y 2015; imágenes de satélite Quickbird de febrero de 2008; análisis granulométricos y morfoscópicos de sedimientos recolectados en los principales accidentes geográficos del area proglacial del glaciar Collins y datos del Modelo de Elevación Digital TanDEM-X. La topografia de la superfície del glaciar Collins fue obtenida por DGNSS a lo largo de 11 años (1997/98-2008/09) y se utilizaron los datos para calculcular el área y el espesor aproximados del glaciar en 2030, 2050 y 2070. Acerca de los resultados, se destaca que el glaciar Collins perdió 1,4km2 en el período PEH. En un escenario de calentamiento atmosférico, utilizando el modelo de índice de derretimiento, el glaciar perderá aproximadamente el 5% de su área total hasta 2030 (0,90 km²), el 21% (3,60 km²) hasta 2050 y el 35% (5, 90 km²) hasta 2070. Se identificaron cuatro sectores en la zona proglacial: el sector 1 presentó cambios enfrente del glaciar desde la PEH, presencia de flutings y morrenas de recesión. El sector 2 presentró una retracción alrededor de 100 metros en el período PEH-2018, con el depósito de morrenas de recesión de cerca de 2 m de altura y de morrenas de empuje de unos 10 metros de altura. El sector 3 presentó 350 metros de retracción desde el PEH, formación de morrenas de recesión y ausencia de morrenas de empuje. El sector 4 presentó 1.500 metros de retracción desde el PEH, formando una morrena de empuje de cerca de 12 metros de altura. Este comportamiento, que ocurre desde la PEH, permite validar el modelo de escenario futuro. Las áreas libres de hielo pueden expandirse 1,4 km² en el período PEH-2070. Considerando el proceso hidrológico y sedimentológico, las áreas más dinámicas serán los sectores 1 y 2, debido al retroceso más rápido del glaciar. Cabe destacar que la zona recientemente libre de hielo del glaciar Collins también estará sujeta a procesos periglaciales que podrán ser analizados solamente mediante una evaluación sistémica, considerando interacciones y cambios en los sistemas hidrológico, sedimentario y biológico. Sin embargo, se estima que los procesos periglaciales probablemente predominarán a lo largo de la primera etapa posterior al retroceso del glaciar Collins, presentando un área inestable, con una alta concentración de sedimentos que forman accidentes geográficos como morrenas, eskers, flutings y canales entrelazados capaces de transportar material para la actual zona proglacial. El área proglacial actual probablemente cambiará debido a la reducción del suministro de agua de deshielo y a una mayor distancia de los glaciales. Cabe señalar que el modelo del índice de derretimiento no considera las variaciones en la temperatura del aire, lo que obviamente puede generar diferencias en los escenarios propuestos. Sin embargo, se destaca que los resultados encontrados en esta investigación son consistentes con los valores de retracción de volumen y de área de los glaciares de la isla Rey Jorge y de la Península Antártica encontrados en otros artículos. Se destaca, también, que los resultados encontrados en esta investigación están de acuerdo con los valores de retracción de volumen y de área de los glaciares de la Isla Rey Jorge y de la Península Antártica encontrados en otros artículos.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[paraglacial adjustment]]></kwd>
<kwd lng="en"><![CDATA[landforms]]></kwd>
<kwd lng="en"><![CDATA[glacier retreat]]></kwd>
<kwd lng="en"><![CDATA[proglacial system]]></kwd>
<kwd lng="es"><![CDATA[ajuste paraglacial]]></kwd>
<kwd lng="es"><![CDATA[accidentes del terreno]]></kwd>
<kwd lng="es"><![CDATA[retroceso glacial]]></kwd>
<kwd lng="es"><![CDATA[sistema proglacial]]></kwd>
</kwd-group>
</article-meta>
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