<?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>S2663-39812019000100033</article-id>
<article-id pub-id-type="doi">10.35424/rcarto.i98.140</article-id>
<title-group>
<article-title xml:lang="pt"><![CDATA[Análise da Evolução Temporal do Datum Vertical Brasileiro de Imbituba]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Silva]]></surname>
<given-names><![CDATA[Luciana Maria Da]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Freitas]]></surname>
<given-names><![CDATA[Sílvio Rogério Correia de]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidade Estadual de Campinas Centro de Estudos de Petróleo ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Brazil</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidade Federal do Paraná Departamento de Geomática ]]></institution>
<addr-line><![CDATA[Curitiba ]]></addr-line>
<country>Brazil</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2019</year>
</pub-date>
<numero>98</numero>
<fpage>33</fpage>
<lpage>57</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2663-39812019000100033&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2663-39812019000100033&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2663-39812019000100033&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="pt"><p><![CDATA[Resumo Atualmente, os temas mais centrais da Geodésia vinculam-se ao provimento de um Sistema de Referência Global único, ao qual possam ser vinculadas de forma unívoca e com acurácia as mudanças globais de caráter geométrico e físico. O Global Geodetic Reference Frame visa a melhor estruturação dos Sistemas de Observação da Terra atualmente com perspectivas da determinação das mudanças globais ao nível de uma parte por bilhão, considerando vários parâmetros geométricos e físicos. Neste contexto pretende-se que o International Height Reference Frame, realização do International Height Reference System, possua consistência global de, pelo menos, um centímetro na sua realização e controle espaço/temporal na ordem do milímetro por ano. Considerando esses aspectos, analisou-se a evolução temporal do Datum Vertical Brasileiro de Imbituba utilizando dados maregráficos do nível do mar obtido de: Permanent Service for Mean Sea Level (1948 a 1968), University of Hawaii Sea Level Center (2001 a 2007) e Rede Maregráfica Permanente para Geodésia (2006 a 2016), e dados de distintas missões altimétricas do período de 1991 a 2015 obtidos do Banco de Dados do Deutsches Geodätisches Forschungsinstitut. Assim como, dados de posicionamento contínuo GNSS do período de 2007 a 2016, da Rede Brasileira de Monitoramento Contínuo, os quais foram utilizados para modelagem dos movimentos locais da crosta. Os resultados permitiram discriminar os movimentos da crosta em relação ao nível do mar. Para isto, utilizou-se a tendência de variação do nível do mar evidenciada pelo marégrafo, bem como a variação da componente vertical obtida com o processamento GNSS e da Sea Surface Height obtida dos dados dos satélites altímetros.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Nowadays, the most central themes of Geodesy are linked to the provision of a unique Global Reference System, to which can be tied of unique form and with sufficient accuracy the geometrical and physical global changes. The Global Geodetic Reference Frame aims at better structuring Earth Observation Systems currently with prospects of the global changes determination at the level of one part per billion, considering several geometric and physical parameters. In this context, it is intended that the International Height Reference Frame, realization of the International Height Reference System, has an overall consistency of at least one centimeter in its realization and space/temporal control in the order of millimeter per year. Considering these aspects, it was analyzed the temporal evolution of the Imbituba Brazilian Vertical Datum utilizing tide gauge data from the sea level obtained from: Permanent Service for Mean Sea Level (1948 to 1968), University of Hawaii Sea Level Center (2001 to 2007) and Permanent Tide Gauge Network for Geodesy (2006 to 2016), and data from different altimetry missions from 1991 to 2015 obtained from the database of the Deutsches Geodätisches Forschungsinstitut. As like as, data obtained from GNSS continuous positioning of period from 2007 to 2016 from Brazilian GNSS Network for Continuous Monitoring, which were used to modeling the local movements of the crust. The results allowed discriminating the crust movements in relation to the sea level. To achieve it, the trend of sea level variation evidenced by the tide gauge was used, as well as the variation of the vertical component obtained with the GNSS processing and the Sea Surface Height obtained from the satellite altimetry data.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Actualmente, los temas más centrales de Geodesia se vinculan a la provisión de un Sistema de Referencia Global único, al que puedan vincularse de forma unívoca y con exactitud los cambios globales de carácter geométrico y físico. El Global Geodetic Reference Frame tiene como objetivo la mejor estructuración de los Sistemas de Observación de la Tierra actualmente con perspectivas de la determinación de los cambios globales al nivel de una parte por mil millones, considerando varios parámetros geométricos y físicos. En este contexto, se pretende que el International Height Reference Frame, realizado por International Height Reference System, posea consistencia global de, por lo menos, un centímetro en su realización y control espacio/temporal en el orden del milímetro por año. Considerando estos aspectos, análisis y evolución temporal del Datum Vertical Brasileño de Imbituba utilizando datos mareográficos del nivel del mar de: Permanent Service for Mean Sea Level (1948 a 1968), University of Hawaii Sea Level Center (2001 a 2007) y Red Mareográfica Permanente para Geodésia (2006 a 2016), y datos de distintas misiones altimétricas del período 1991 a 2015 obtenidos del Banco de Datos del Deutsches Geodätisches Forschungsinstitut. Así como, datos de posicionamiento continuo GNSS del período de 2007 a 2016, de la Red Brasileña de Monitoreo Continuo, los cuales fueron utilizados para modelado de los movimientos locales de la corteza. Los resultados permitirán discriminar los movimientos de la corteza en relación al nivel del mar. Para esto, se utilizó la tendencia de variación del nivel del mar evidenciado por el mareógrafo, así como la variación del componente vertical obtenido con el procesamiento GNSS y de la Sea Surface Height obtenida de los datos de los satélites altimétricos.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Brazilian vertical datum]]></kwd>
<kwd lng="en"><![CDATA[tide gauge]]></kwd>
<kwd lng="en"><![CDATA[satellite altimetry]]></kwd>
<kwd lng="en"><![CDATA[GNSS continuous data]]></kwd>
<kwd lng="en"><![CDATA[mean sea level]]></kwd>
<kwd lng="pt"><![CDATA[Datum vertical brasileiro]]></kwd>
<kwd lng="pt"><![CDATA[marégrafo]]></kwd>
<kwd lng="pt"><![CDATA[altimetria por satélite]]></kwd>
<kwd lng="pt"><![CDATA[dados contínuos GNSS]]></kwd>
<kwd lng="pt"><![CDATA[nível médio do mar]]></kwd>
<kwd lng="es"><![CDATA[Datum vertical brasileño]]></kwd>
<kwd lng="es"><![CDATA[mareógrafo]]></kwd>
<kwd lng="es"><![CDATA[altimetría por satélite]]></kwd>
<kwd lng="es"><![CDATA[dados continuos GNSS]]></kwd>
<kwd lng="es"><![CDATA[nivel medio del mar]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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