<?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>0185-3880</journal-id>
<journal-title><![CDATA[Ciencias marinas]]></journal-title>
<abbrev-journal-title><![CDATA[Cienc. mar]]></abbrev-journal-title>
<issn>0185-3880</issn>
<publisher>
<publisher-name><![CDATA[Universidad Autónoma de Baja California, Instituto de Investigaciones Oceanológicas]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0185-38802017000300191</article-id>
<article-id pub-id-type="doi">10.7773/cm.v43i3.2775</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Current variability by wave propagation in Todos Santos Bay, Baja California, Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Variabilidad de corrientes por propagación de ondas en bahía de Todos Santos, Baja California, México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mateos]]></surname>
<given-names><![CDATA[Efrain]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Marinone]]></surname>
<given-names><![CDATA[Silvio Guido]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,IMTA Instituto Mexicano de Tecnología del Agua  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Centro de Investigación Cienctifica y de Educación Superior de Ensenada  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<volume>43</volume>
<numero>3</numero>
<fpage>191</fpage>
<lpage>201</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802017000300191&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802017000300191&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802017000300191&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract   The temperature, velocity, and sea level fields for a summer climatological month (August) were analyzed using tridimensional and baroclinic model outputs in Todos Santos Bay (TSB), Baja California, Mexico. The numerical model was forced with wind (non-stationary), heat flux, and California Current System climatology on the open boundary. The 3- to 5-day current variability is related to a baroclinic wave traveling towards the northwest of the bay. Wave travel periodicity was due to the release of accumulated water from the Ensenada-Punta Banda Estuary (E-PBE) region. Local wind stress causes southeastward water flow and, given the TSB geometry, water accumulates in the E-PBE region. Weakening wind stress was the main cause of water release. In addition, complex empirical orthogonal function analysis found that outer TSB disturbances cause sea level variability.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen A partir de las salidas de un modelo tridimensional y baroclínico, se analizaron los campos de temperatura, velocidad y superficie libre del mar para un mes climatológico de verano (agosto) en la bahía de Todos Santos (BTS), Baja California, México. El modelo numérico se forzó con viento (no estacionario), flujos de calor y en las fronteras abiertas con climatología que incluyó al Sistema de la Corriente de California. Se encontró que la variabilidad, de 3 a 5 días, del campo de velocidad está relacionado con la propagación, hacia el noroeste de la bahía, de una onda baroclínica. La periodicidad de la propagación de la onda se debió a la liberación de agua acumulada en la región entre Ensenada y el estero de Punta Banda (E-EPB). Se encontró que el esfuerzo del viento local es la causa del transporte de agua hacia el sureste, y debido a la geometría de la BTS, el agua se acumula en la región E-EPB. La relajación del esfuerzo del viento fue la principal causa de la liberación de agua acumulada. A partir del análisis de funciones empíricas ortogonales complejas, se encontró que también las perturbaciones provenientes del exterior de la BTS causan variabilidad en la superficie libre del mar.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Todos Santos Bay]]></kwd>
<kwd lng="en"><![CDATA[subinertial wave travel]]></kwd>
<kwd lng="es"><![CDATA[bahía de Todos Santos]]></kwd>
<kwd lng="es"><![CDATA[propagación de ondas subinerciales]]></kwd>
</kwd-group>
</article-meta>
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