<?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>2663-3981</journal-id>
<journal-title><![CDATA[Revista cartográfica]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. cartogr.]]></abbrev-journal-title>
<issn>2663-3981</issn>
<publisher>
<publisher-name><![CDATA[Instituto Panamericano de Geografía e Historia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2663-39812021000100069</article-id>
<article-id pub-id-type="doi">10.35424/rcarto.i102.835</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Determinación del nivel medio del mar en el mar de Bransfield. Aplicación a la determinación del geoide en islas Decepción y Livingston, Islas Shetland del Sur (Antártida)]]></article-title>
<article-title xml:lang="en"><![CDATA[Determination of the Mean Sea Level in the Bransfield Sea. Application to determination of the geoid at Deception and Livingston islands (Antarctica)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jigena Antelo]]></surname>
<given-names><![CDATA[Bismarck]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Berrocoso Domínguez]]></surname>
<given-names><![CDATA[Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vidal Pérez]]></surname>
<given-names><![CDATA[Juan Manuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Cádiz Departamento de Ciencias y Técnicas de la Navegación y Construcciones Navales ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Cádiz Facultad de Ciencias Laboratorio de Astronomía, Geodesia y Cartografía]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Cádiz Escuela de Ingeniería Naval y Oceánica ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<numero>102</numero>
<fpage>69</fpage>
<lpage>97</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2663-39812021000100069&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2663-39812021000100069&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2663-39812021000100069&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Este trabajo presenta un estudio detallado para la determinación del nivel medio del mar (NMM), las constituyentes de marea y un geoide de precisión en las islas Decepción y Livingston y el entorno del mar de Bransfield. Para realizar estos trabajos es necesario definir el marco de referencia geodésico, para ello se han utilizaron las redes geodésicas REGID (Red Geodésica de Isla Decepción), RENID (Red de Nivelación de Isla Decepción) y REGRID (Red Gravimétrica de Isla Decepción), utilizando como vértices fundamentales algunos puntos pertene-cientes a la red RGAE (Red Geodésica Antártica Española). Los datos de marea fueron obtenidos mediante sensores de presión instalados en las estaciones mareográficas de LIVMAR y DECMAR, islas Livingston y Decepción respectivamente, ubicadas muy cerca de las bases antárticas y Gabriel de Castilla. Se obtuvieron las primeras series temporales con 798 días de observación en ambas estaciones, cuyo análisis armónico nos proporcionó 70 constituyentes de marea, siendo 19 las más representativas con amplitudes superiores a 1 cm. Se determinamos el nivel medio del mar, utilizando como puntos fundamentales el LN00 (isla Decepción) y BEJC (isla Livingston). Por último, se determinó el modelo de geoide de precisión, GeoiDEC14, calculado a partir de mediciones GPS, gravimétricas y de nivelación y cuyo resultado ha sido contrastado con los modelos globales más actuales. Estos son los primeros resultados de determinación del nivel medio del mar y la obtención de un modelo de geoide de precisión en esta zona de la Antártida y mejoran trabajos previos realizados en la región.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: This work presents a detailed study in order to determine the mean sea level (NMM), the tidal constituents and a precision geoid at Deception and Livingston Islands and the Bransfield Sea area. To carry out these works, it is necessary to define the geodetic reference frame, for this the geodetic networks like REGID (Geodetic network of Deception Island), RENID (Levelling network of Deception Island) and REGRID (Gravimetric network of Deception Island) have been used. In addition, some geodesic points belonging to the RGAE network (Spanish Antarctic Geodetic network) as fundamental vertices, were used. The tidal data were obtained using pressure sensors installed at the LIVMAR and DECMAR tidal stations, Livingston and Deception islands, respectively, located very close to the Antarctic Bases and &#8220;Juan Carlos I&#8221; and Gabriel de Castilla. The first time series were obtained with 798 days of observation in both stations, whose harmonic analysis provided us with 70 tidal constituents, 19 being the most representative with amplitudes greater than 1 cm. With these tidal series we determine the mean sea level, using the LN00 (Deception Island) and BEJC (Livingston island) as a fundamental points. Finally, the precision geoid model, GeoiDEC14, was determined from GPS, gravimetric and leveling measurements. To contrast the results, a comparison of GeoiDEC14 against the most current global models, was made. These are the first results of determining the mean sea level and obtaining a precision geoid model in this Antarctic area. The results obtained improve previous work carried out in the region.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[ondulación del geoide]]></kwd>
<kwd lng="es"><![CDATA[gravimetría]]></kwd>
<kwd lng="es"><![CDATA[nivelación]]></kwd>
<kwd lng="es"><![CDATA[constituyentes de marea]]></kwd>
<kwd lng="es"><![CDATA[Base Antártica Española]]></kwd>
<kwd lng="en"><![CDATA[Geoid undulation]]></kwd>
<kwd lng="en"><![CDATA[gravimetry]]></kwd>
<kwd lng="en"><![CDATA[leveling]]></kwd>
<kwd lng="en"><![CDATA[tide constituents]]></kwd>
<kwd lng="en"><![CDATA[Spanish Antarctic Base]]></kwd>
</kwd-group>
</article-meta>
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