<?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>0012-7353</journal-id>
<journal-title><![CDATA[DYNA]]></journal-title>
<abbrev-journal-title><![CDATA[Dyna rev.fac.nac.minas]]></abbrev-journal-title>
<issn>0012-7353</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0012-73532019000400017</article-id>
<article-id pub-id-type="doi">10.15446/dyna.v86n211.80375</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Dynamics of physicochemical variables of the northern Colombian Caribbean coastal waters]]></article-title>
<article-title xml:lang="es"><![CDATA[Dinámica de variables fisicoquímicas de las aguas costeras del Caribe norte colombiano]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vega-Sequeda]]></surname>
<given-names><![CDATA[Johanna]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Polo-Silva]]></surname>
<given-names><![CDATA[Carlos Julio]]></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[Paramo-Granados]]></surname>
<given-names><![CDATA[Jorge]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sanjuan-Muñoz]]></surname>
<given-names><![CDATA[Adolfo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Bogotá Jorge Tadeo Lozano Facultad de Ciencias Naturales e Ingeniería ]]></institution>
<addr-line><![CDATA[Santa Marta ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad del Magdalena Grupo de Investigación Ciencia y Tecnología Pesquera Tropical (CITEPT) ]]></institution>
<addr-line><![CDATA[Santa Marta ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>86</volume>
<numero>211</numero>
<fpage>17</fpage>
<lpage>25</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0012-73532019000400017&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0012-73532019000400017&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0012-73532019000400017&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract This study explored oceanographic dynamics related to high productivity processes in the northern Colombian Caribbean. Four scientific expeditions were carried out between May and December 2018, where selected physicochemical variables were measured using a CTDO (conductivity, temperature and dissolved oxygen sensor system), and transparency with a Secchi disc. May and December showed typical upwelling waters, while August and November showed waters characteristic of the rainy season. Spatial dynamics were related to temperature and salinity. Thus, northeastern stations showed colder and saltier surface waters compared to those located to the southwest. Vertical readings were taken and the Caribbean Surface Water mass was identified, and below it the subtropical subsurface water mass, which emerges at the beginning of the year. The results suggest that upwelling and freshwater runoff have a direct impact on the hydrographic structure of the region.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se evaluó la dinámica oceanográfica relacionada con los procesos de alta productividad en el Caribe norte colombiano. Se realizaron cuatro cruceros científicos entre mayo y diciembre de 2018, en los que se midieron la temperatura, la salinidad y el oxígeno con una sonda CTDO y transparencia con un disco Secchi. Mayo y diciembre presentaron aguas típicas de afloramientos con menor intensidad, mientras que agosto y noviembre tuvieron aguas características de la época lluviosa. La dinámica espacial estuvo relacionada con la temperatura y la salinidad. Las estaciones del noreste presentaron aguas superficiales más frías y salinas, en relación con las localizadas hacia el suroeste. A nivel vertical, se identificó la masa de agua superficial del Caribe, y debajo la masa de agua subsuperficial subtropical que aflora a inicios de año. Los resultados sugieren que la surgencia y los aportes de agua dulce tienen un impacto directo sobre la estructura hidrográfica de la región.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[upwelling]]></kwd>
<kwd lng="en"><![CDATA[physicochemical variables]]></kwd>
<kwd lng="en"><![CDATA[water masses]]></kwd>
<kwd lng="en"><![CDATA[northern Colombian Caribbean]]></kwd>
<kwd lng="es"><![CDATA[surgencia]]></kwd>
<kwd lng="es"><![CDATA[variables fisicoquímicas]]></kwd>
<kwd lng="es"><![CDATA[masas de agua]]></kwd>
<kwd lng="es"><![CDATA[Caribe norte colombiano]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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