<?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>0187-6236</journal-id>
<journal-title><![CDATA[Atmósfera]]></journal-title>
<abbrev-journal-title><![CDATA[Atmósfera]]></abbrev-journal-title>
<issn>0187-6236</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Ciencias de la Atmósfera y Cambio Climático]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0187-62362023000200207</article-id>
<article-id pub-id-type="doi">10.20937/atm.53093</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Cyclonic circulation and climatology of SST, CHL and wind stress curl in a semi-enclosed bay (Bahía de La Paz, Gulf of California, Mexico)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Beier]]></surname>
<given-names><![CDATA[Emilio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castro]]></surname>
<given-names><![CDATA[Rubén]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Godínez]]></surname>
<given-names><![CDATA[Víctor M.]]></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 Laboratorio de Macroecología Marina ]]></institution>
<addr-line><![CDATA[La Paz Baja California Sur]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Baja California (UABC) Facultad de Ciencias Marinas ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Centro de Investigación Científica y de Educación Superior de Ensenada Departamento de Oceanografía Física ]]></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>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>36</volume>
<numero>2</numero>
<fpage>207</fpage>
<lpage>224</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362023000200207&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362023000200207&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362023000200207&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The first direct current observations (with the Lowering Acoustic Doppler Current Profiler [LADCP] and surface drifters) in Bahía de La Paz, in the southwestern Gulf of California (GC), concur with previous reports that the main dynamical feature during summer is a closed cyclonic circulation. However, we found that geostrophic calculations overestimate the speed of the orbital velocity: actual speeds (0.20-0.25 m s-1) were ~25-40% lower than those estimated from geostrophic balance (0.25-0.35 m s-1). The reason is that the centrifugal force cannot be neglected in this case. The mean rotation period during ship-borne observations in August 2004 was ~1.4 days, but it varied in the time that surface drifters were inside the bay, from ~1-2 days in June-July to ~2.5-3 days in September-October. The analysis of satellite data (wind velocity, sea surface temperature and chlorophyll) shows that from May to September the wind stress curl is strong and cyclonic, and the surface of the bay is cooler and richer than the adjacent Gulf of California waters, which could be attributed to the positive wind stress curl. This positive wind stress curl on the bay is part of a larger-scale positive wind stress curl distribution that surrounds the southern part of the Baja California Peninsula during summer, probably enhanced in the bay by local topography features. Although there is an exchange of water between the bay and the GC, its effect on the dynamics is poorly known.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Las primeras observaciones directas de corrientes (con el Perfilador de Corriente Acústico Doppler y derivadores superficiales) en la Bahía de La Paz, situada al suroeste del Golfo de California (GC), coinciden con estudios anteriores en que la principal característica dinámica durante el verano es una circulación ciclónica cerrada. Sin embargo, encontramos que los cálculos goestróficos sobrestiman a las velocidades de rotación: las velocidades observadas (0.20-0.25 m s-1) fueron ~25-40% más bajas que las estimadas a partir del balance geostrófico (0.25-0.35 m s-1). La razón es que en este caso no se puede despreciar la fuerza centrífuga. El período medio de rotación durante las observaciones a bordo del buque en agosto de 2004 fue de ~1.4 días, pero varió durante el tiempo en que los derivadores estuvieron en la bahía, de ~1-2 días en junio-julio a 2.5-3 días en septiembre-octubre. Los análisis satelitales (velocidad del viento, temperatura superficial del mar y clorofila) muestran que, de mayo a septiembre, el rotacional del esfuerzo del viento fue intenso y ciclónico, y la superficie de la bahía fue más fría y más rica que las aguas adyacentes del golfo, lo cual puede atribuirse al rotacional del esfuerzo del viento positivo. Este rotacional del esfuerzo del viento positivo sobre la bahía, es parte de una distribución del rotacional del esfuerzo del viento positivo de mayor escala que rodea la parte sur de la península de Baja California durante el verano, probablemente aumentado en la bahía por las características topográficas locales. Aunque existe un intercambio de agua entre la bahía y el GC, su efecto sobre la dinámica es poco conocido.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[cyclonic circulation]]></kwd>
<kwd lng="en"><![CDATA[current observations (LADCP]]></kwd>
<kwd lng="en"><![CDATA[drifters buoys)]]></kwd>
<kwd lng="en"><![CDATA[wind stress curl]]></kwd>
<kwd lng="en"><![CDATA[Bahía de La Paz]]></kwd>
</kwd-group>
</article-meta>
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