<?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>0188-4611</journal-id>
<journal-title><![CDATA[Investigaciones geográficas]]></journal-title>
<abbrev-journal-title><![CDATA[Invest. Geog]]></abbrev-journal-title>
<issn>0188-4611</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geografía]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0188-46112025000200103</article-id>
<article-id pub-id-type="doi">10.14350/rig.61045</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Tendencias 1953-2018 de la humedad atmosférica en la parte norte del mar de Cortés a partir de cuatro fuentes de datos]]></article-title>
<article-title xml:lang="en"><![CDATA[Trends in atmospheric humidity in the northern Gulf of California from 1953 to 2018 based on four data source]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tejeda-Martínez]]></surname>
<given-names><![CDATA[Adalberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Baruch-Vera]]></surname>
<given-names><![CDATA[Aranza Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Parra]]></surname>
<given-names><![CDATA[Raquel Elisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gómez-Díaz]]></surname>
<given-names><![CDATA[René Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castro-Díaz]]></surname>
<given-names><![CDATA[Jaime Omar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Veracruzana Facultad de Instrumentación Electrónica ]]></institution>
<addr-line><![CDATA[Xalapa-Enríquez Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Veracruzana Facultad de Instrumentación Electrónica ]]></institution>
<addr-line><![CDATA[Xalapa-Enríquez Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Veracruzana Facultad de Instrumentación Electrónica ]]></institution>
<addr-line><![CDATA[Xalapa-Enríquez Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Veracruzana Facultad de Instrumentación Electrónica ]]></institution>
<addr-line><![CDATA[Xalapa-Enríquez Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad Veracruzana Facultad de Instrumentación Electrónica ]]></institution>
<addr-line><![CDATA[Xalapa-Enríquez Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<numero>117</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0188-46112025000200103&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0188-46112025000200103&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0188-46112025000200103&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se evaluaron las tendencias de temperatura, humedad relativa y humedad absoluta en la isla Rasa, Baja California, ubicada en el centro del Mar de Cortés. Las tendencias de las variables hígricas se obtuvieron de: a) la estación meteorológica automática de Bahía de los Ángeles (28.94°N, 113.55°W y 4 msnm; EMAA), periodo 2001-2019; b) estimaciones a partir de la temperatura mínima de las estaciones climatológicas de El Barril (28.30°N, 112.88°W, 20 msnm), Bahía de Kino (28.82°N, 111.93°W, 2 msnm) y Bahía de los Ángeles (28.94°N, 113.55°W, 4 msnm), periodo 1953-2018; c) estimaciones bajo la hipótesis de la humedad relativa invariante ante el calentamiento (o enfriamiento) local y global; d) datos de reanálisis de temperatura y temperatura de punto de rocío a 2 m de altura para las coordenadas de la isla. Las tendencias de humedad absoluta resultaron muy bajas e inversas entre los diferentes métodos de obtención de la variable y su tendencia regional estimada es positiva, pero insignificante. La tendencia de humedad relativa a partir de los datos de reanálisis fue de 0.18 puntos porcentuales por década y para la humedad absoluta de 0.25 gm-3/década. Como conclusión, en el centro del mar de Cortés las tendencias de humedad son inciertas e insignificantes comparadas con las medias climáticas de la zona. La tendencia térmica resultó de 0.36 °C/década para la EMAA, la tendencia regional fue de 0.21 °C/década y la obtenida con datos de reanálisis de 0.29 °C/década, todas similares a la global reportada por el IPCC.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Temperature, relative humidity, and absolute humidity trends were evaluated on Rasa Island, Baja California, located in the center of the Sea of Cortez. The trends in hygric variables were obtained from: a) the automatic weather station in Bahía de los Ángeles (28.94°N, 113.55°W and 4 m above sea level; EMAA), period 2001-2019; b) estimates based on the minimum temperature of the weather stations in El Barril (28.30°N, 112.88°W, 20 m above sea level), Bahía de Kino (28.82°N, 111.93°W, 2 m above sea level) and Bahía de los Ángeles (28.94°N, 113.55°W, 4 m above sea level), period 1953-2018; c) estimates under the hypothesis of relative humidity invariant to local and global warming (or cooling); d) reanalysis data for temperature and dew point temperature at 2 m above sea level for the island's coordinates. Absolute humidity trends were very low and inverse between the different methods of obtaining the variable, and their estimated regional trend is positive but insignificant. The relative humidity trend based on reanalysis data was 0.18 percentage points per decade and for absolute humidity 0.25 gm-3/decade. In conclusion, in the center of the Sea of Cortez, humidity trends are uncertain and insignificant compared to the climate averages for the area. The temperature trend was 0.36 °C/decade for the EMAA, the regional trend was 0.21 °C/decade, and the trend obtained from reanalysis data was 0.29 °C/decade, all similar to the global trend reported by the IPCC.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[temperatura]]></kwd>
<kwd lng="es"><![CDATA[humedad absoluta]]></kwd>
<kwd lng="es"><![CDATA[humedad relativa]]></kwd>
<kwd lng="es"><![CDATA[estimaciones]]></kwd>
<kwd lng="es"><![CDATA[reanálisis]]></kwd>
<kwd lng="es"><![CDATA[tendencias]]></kwd>
<kwd lng="en"><![CDATA[temperature]]></kwd>
<kwd lng="en"><![CDATA[relative humidity]]></kwd>
<kwd lng="en"><![CDATA[absolute humidity]]></kwd>
<kwd lng="en"><![CDATA[estimations]]></kwd>
<kwd lng="en"><![CDATA[reanalysis]]></kwd>
<kwd lng="en"><![CDATA[trends]]></kwd>
</kwd-group>
</article-meta>
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