<?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>S0185-38802018000100001</article-id>
<article-id pub-id-type="doi">10.7773/cm.v44i1.2743</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Effects of seasonal and interannual events on satellite-derived phytoplankton biomass and production in the southernmost part of the California Current System during 2003-2016]]></article-title>
<article-title xml:lang="es"><![CDATA[Efectos de eventos estacionales e interanuales en la biomasa y producción fitoplanctónicas derivadas de satélite en el extremo sur del Sistema de la Corriente de California en el periodo 2003-2016]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortiz-Ahumada]]></surname>
<given-names><![CDATA[José Carlos]]></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[Gómez-Valdés]]></surname>
<given-names><![CDATA[Jose]]></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>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<volume>44</volume>
<numero>1</numero>
<fpage>1</fpage>
<lpage>20</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0185-38802018000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0185-38802018000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0185-38802018000100001&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract We characterized the spatial and temporal variations of sea surface temperature (SST), satellite-derived chlorophyll a (Chlsat) concentration, and phytoplankton production (PP) along two 300-km long transects in the southernmost part of the California Current System, one off Cabo San Lázaro (TCSLa) and the other off Cabo San Lucas (TCSLu). Moderate Resolution Imaging Spectroradiometer (Aqua-MODIS) SST and DDoi: Chlsat monthly composites and PP monthly composites were used for the 2003-2016 period. An &#8220;average year&#8221; was generated for each transect and each variable, as an approximation to the climatology. The Chlsat and PP values were higher in the inshore area than in the offshore area: 4.0 mg·m-3 and 4.5 g Cm-2·d-1, respectively, for the inshore area of TCSLa and 1.4 mg·m-3 and 1.8 g C·m-2·d-1, respectively, for the inshore area of TCSLu; ~0.1 mg·m-3 and 0.4 g C·m-2·d-1, respectively, for the offshore area of both transects. In general, SST showed minimum values (~17.0 ºC) in the inshore area and maximum values (~29.4 ºC) in the offshore area. Chlsat values in the coastal zone were higher on TCSLa than on TCSLu, but offshore Chlsat values were often higher on TCSLu than on TCSLa. Seasonal and interannual variations were observed on both transects, but the seasonal variations were dominant. The effects of &#8220;the Blob&#8221; in 2014 and of the 2015-2016 eastern Pacific type of El Niño were similarly strong off both capes but caused no collapse in phytoplankton biomass, which decreased to only approximately half the values for the non-El Niño years. The 2003 and 2010 central Pacific type of El Niño events also had strong impacts. The 2005 central Pacific type of El Niño had a strong impact on the biology of TCSLu, like the impact of the 2014 and 2015-2016 events, but not on the biology of TCSLa. The coastal dynamics in the California Current System show spatial variations; thus, seasonal and interannual events have different effects at different geographic locations.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se caracterizó la variación espaciotemporal de la temperatura superficial del mar (TSM), la concentración de clorofila a derivada de satélite (Chlsat) y la producción primaria (PP) en el extremo sur del Sistema de la Corriente de California, en 2 transectos de 300 km de largo, uno frente a cabo San Lázaro (TCSLa) y otro frente a cabo San Lucas (TCSLu). Se utilizaron composiciones mensuales de TSM y Chlsat del sensor Moderate Resolution Imaging Spectroradiometer (Aqua-MODIS) y composiciones mensuales de PP, para el periodo 2003-2016. Se generó un &#8220;año promedio&#8221; para cada transecto y cada variable como aproximación a la climatología. Los valores de Chlsat y PP fueron mayores en la zona costera que en la zona oceánica: 4.0 mg·m-3 y 4.5 g C·m-2·d-1, respectivamente, para la zona costera de TCSLa y 1.4 mg·m-3 y 1.8 g C·m-2·d-1, respectivamente, para la zona costera de TCSLu; ~0.1 mg·m-3 y 0.4 g C·m-2·d-1, respectivamente, para la zona oceánica de ambos transectos. En general, la TSM presentó los valores mínimos en la zona costera (~17.0 ºC) y los máximos en la zona oceánica (~29.4 ºC). Los valores de Chlsat en la zona costera fueron mayores en TCSLa que en TCSLu, pero la Chlsat en la zona oceánica a menudo fue mayor en TCSLu que en TCSLa. Hubieron variaciones estacionales e interanuales en ambos transectos, pero las variaciones estacionales fueron dominantes. Los efectos de &#8220;El Blob&#8221; de 2014 y El Niño del tipo Pacífico oriental de 2015-2016 fueron similarmente fuertes frente a ambos cabos, pero no hubo un colapso de la biomasa fitoplanctónica, la cual sólo disminuyó a aproximadamente la mitad de los valores de años sin El Niño. Los eventos El Niño del tipo Pacífico central de 2003 y 2010 también tuvieron impactos fuertes. El Niño del tipo Pacífico central de 2005 tuvo un impacto fuerte en la biología de TCSLu, similar al impacto de los eventos de 2014 y 2015-2016, pero no en la biología de TCSLa. Las variaciones espaciales de la dinámica costera del Sistema de la Corriente de California causan que los eventos estacionales e interanuales tengan diferentes efectos en localidades geográficas diferentes.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[California Current System]]></kwd>
<kwd lng="en"><![CDATA[satellite data]]></kwd>
<kwd lng="en"><![CDATA[phytoplankton biomass]]></kwd>
<kwd lng="en"><![CDATA[phytoplankton production]]></kwd>
<kwd lng="en"><![CDATA[spatiotemporal variation]]></kwd>
<kwd lng="es"><![CDATA[Sistema de la Corriente de California]]></kwd>
<kwd lng="es"><![CDATA[datos satelitales]]></kwd>
<kwd lng="es"><![CDATA[biomasa fitoplanctónica]]></kwd>
<kwd lng="es"><![CDATA[producción fitoplanctónica]]></kwd>
<kwd lng="es"><![CDATA[variación espaciotemporal]]></kwd>
</kwd-group>
</article-meta>
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