<?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>S0185-38802017000300137</article-id>
<article-id pub-id-type="doi">10.7773/cm.v43i3.2707</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Temporal variations of water pCO2 and the air-water CO2 flux at a coastal location in the southern California Current System: diurnal to interannual scales]]></article-title>
<article-title xml:lang="es"><![CDATA[Variaciones temporales de pCO2 del agua y flujos aire-agua de CO2 en una localidad costera en el sur del Sistema de la Corriente de California: de la escala diurna a la interanual]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Coronado-Álvarez]]></surname>
<given-names><![CDATA[Luz de Lourdes Aurora]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Álvarez-Borrego]]></surname>
<given-names><![CDATA[Saúl]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lara-Lara]]></surname>
<given-names><![CDATA[José Rubén]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Solana-Arellano]]></surname>
<given-names><![CDATA[Elena]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Ayón]]></surname>
<given-names><![CDATA[José Martín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zirino]]></surname>
<given-names><![CDATA[Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada  ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Baja California Instituto de Investigaciones Oceanológicas ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,University of California Scripps Institution of Oceanography ]]></institution>
<addr-line><![CDATA[La Jolla California]]></addr-line>
<country>USA</country>
</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>137</fpage>
<lpage>156</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802017000300137&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802017000300137&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802017000300137&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The aim of this work was to identify processes that cause surface CO2 partial pressure (pCO2W) and air-water CO2 flux (FCO2) variations at a coastal location in the California Current System, from semidiurnal to interannual time scales. Such processes may include sea breeze, upwelling, El Niño/Southern Oscillation (ENSO) cycle, and &#8220;The Blob&#8221; (strong positive temperature anomalies in the NE Pacific). Sea surface temperature (SST, 2008-2014) and pCO2W (2008-2015) time series were generated with data collected from a MAPCO2 buoy anchored at 100 m depth and 5 km from Punta Banda (31.6ºN, 116.6ºW), Baja California, México. There were significant changes in SST, pCO2W, and FCO2 that lasted periods that were as short as a few hours and as large as interannual time frames. Spectral analysis showed significant semidiurnal, diurnal, ~15-d, and ~28-d components of variation. Time series were divided into periods according to the Multivariate ENSO Index and the Blob event. Bayesian t tests show that both pCO2W and FCO 2 had high credibility of being different between periods. During La Niña conditions (2010-2011), maximum pCO2W and FCO2 values were higher, and the minimum values were lower, than during &#8220;normal,&#8221; El Niño, and Blob conditions. The pCO2W range during this La Niña event was from 131 to 864 &#956;atm, and the FCO2 range was from -6.9 to 40.4 mmol C m-2 d-1. The FCO2 range during the Blob was from near equilibrium to ~2.5 mmol C m-2 d-1. The extreme values for the FCO2 integral (± standard error), for all periods, were -57.0 ± 0.01 mmol C m-2 for El Niño, and 257.0 ± 0.03 mmol C m-2 for La Niña. The mean FCO2 value (± standard error) was 0.04 ± 0.02 mol C m-2 yr-1. The buoy location was found to be a very weak source of CO2 during the study period.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El objetivo de este trabajo fue identificar los procesos que causan variaciones en periodos de los semidiurnos a los interanuales en la presión parcial superficial de CO2 (pCO2W) y en el flujo de CO2 (FCO2) entre el océano y la atmósfera en una localidad costera del Sistema de la Corriente de California. Tales procesos pueden incluir brisas marinas, surgencias, ciclos El Niño/Oscilación del Sur (ENOS) y el &#8220;Blob&#8221; (grandes anomalías positivas de temperatura en el Pacífico nororiental). Se generaron series de tiempo de temperatura superficial del mar (TSM, 2008-2014) y pCO2W (2008-2015) con datos recuperados de una boya MAPCO2 anclada a 100 m de profundidad y a 5 km de punta Banda (31.6ºN, 116.6ºW), Baja California, México. Se observaron cambios significativos en TSM, pCO2W y FCO2 que duraron periodos tan cortos como de horas y tan largos como de segmentos interanuales. El análisis espectral mostró componentes de variación significativos semidiurnos, diurnos, de ~15 d y de ~28 d. Las series de tiempo fueron divididas en periodos de acuerdo con el Índice Multivariado del ENOS y el Blob. Los resultados de la prueba t bayesiana mostraron que tanto pCO2W como FCO2 tienen alta credibilidad de ser diferentes entre periodos. En 2010-2011, bajo condiciones La Niña, los máximos de pCO2W y FCO2 fueron mayores, y los mínimos menores, que durante condiciones &#8220;normales&#8221;, El Niño y el Blob, con un rango de 131 a 864 &#956;atm para pCO2W y de -6.9 a 40.4 mmol C m-2 d-1 para FCO2. El rango para FCO2 durante el Blob fue de cerca del equilibrio a ~2.5 mmol C m-2 d-1. Los extremos de la integral de FCO2 (± error estándar), para periodos completos, fueron -57.0 ± 0.01 mmol C m-2 para El Niño y 257.0 ± 0.03 mmol C m-2 para La Niña. La media de FCO2 fue 0.04 ± 0.02 mol C m-2 año-1. La localidad de la boya fue una fuente muy débil de CO2 durante el periodo de estudio.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[California Current System]]></kwd>
<kwd lng="en"><![CDATA[CO2 partial pressure]]></kwd>
<kwd lng="en"><![CDATA[CO2 air-water flux]]></kwd>
<kwd lng="en"><![CDATA[coastal zone]]></kwd>
<kwd lng="es"><![CDATA[Sistema de la Corriente de California]]></kwd>
<kwd lng="es"><![CDATA[presión parcial del CO2]]></kwd>
<kwd lng="es"><![CDATA[flujos aire-agua de CO2]]></kwd>
<kwd lng="es"><![CDATA[zona costera]]></kwd>
</kwd-group>
</article-meta>
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