<?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>S0187-62362018000200143</article-id>
<article-id pub-id-type="doi">10.20937/atm.2018.31.02.03</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Fog collection and its relationship with local meteorological variables in a semiarid zone in Chile]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Montecinos]]></surname>
<given-names><![CDATA[Sonia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cereceda]]></surname>
<given-names><![CDATA[Pilar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rivera]]></surname>
<given-names><![CDATA[Daniela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de La Serena Departamento de Física y Astronomía ]]></institution>
<addr-line><![CDATA[La Serena ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Arturo Prat Centro de Estudios Recursos de Energía ]]></institution>
<addr-line><![CDATA[Iquique ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Pontificia Universidad Católica de Chile Centro del Desierto de Atacama ]]></institution>
<addr-line><![CDATA[Santiago ]]></addr-line>
<country>Chile</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>31</volume>
<numero>2</numero>
<fpage>143</fpage>
<lpage>153</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362018000200143&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362018000200143&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362018000200143&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In semiarid and arid zones, fog is considered an important alternative water source. The Southeast Pacific anticyclone and the cold Humboldt Current that characterize the north of Chile promote the formation of stratocumulus along the coastline. The thermally induced winds move these clouds eastwards favoring the formation of fog in the high hills of the Coast Range. The goal of this work is to characterize the fog water collected by a standard fog collector and its relationship with local meteorological variables. We found that the collected water is seasonally dependent, larger in summer than in winter. The mean diurnal cycle in autumn, summer and winter presents two maxima, at the early morning and late afternoon, meanwhile in winter it presents smooth variations during the day. The wind regime was compatible with land-sea circulation. The monthly mean temperature reached the maximum value in March and the minimum value between July and September, whereas the mean monthly daily temperature amplitude was larger in winter than in summer. The minimum values of relative humidity were achieved in the winter months. The fog water collection varies from zero to a maximum value that increased with wind speed, and mainly occurred with SW and NE winds. The fog index (FI) was defined as the percentage of foggy-days per month for which the water collected is greater than one liter. We found that FI follows the same trend as the monthly collected water, and decreases with the mean monthly daily temperature amplitude.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En zonas áridas y semiáridas la niebla es considerada un importante recurso hídrico alternativo. El anticiclón del Pacífico Sudeste y la corriente fría de Humboldt que caracteriza al norte de Chile promueve la formación de estratocúmulos a lo largo de la línea de costa. Los vientos térmicamente inducidos mueven estas nubes hacia el este favoreciendo la formación de niebla en las cumbres altas de la Cordillera de la Costa. El objetivo de este trabajo es caracterizar el agua recolectada por un colector estándar y su relación con las características meteorológicas locales. Encontramos que el agua recolectada depende de la estación del año, siendo mayor en verano que en invierno. El ciclo diario promedio en otoño, primavera y verano presenta dos máximos, uno en la madrugada y el otro en la tarde, mientras que en invierno presenta pocas variaciones durante el día. El régimen de viento es compatible con la circulación mar-tierra. El promedio mensual de temperatura alcanza el máximo valor en marzo y el mínimo entre julio y septiembre. El promedio mensual de la amplitud diaria de la temperatura es mayor en invierno que en verano. El promedio mensual de humedad relativa alcanza el valor mínimo en junio. La recolección de agua de niebla varía desde cero hasta un valor máximo que depende de la rapidez del viento, y ocurre principalmente con vientos del suroeste y noreste. El índice de niebla (FI, por sus siglas en inglés) se define como el porcentaje de días de niebla por mes, en el cual el agua recolectada es mayor que un litro. Encontramos que el FI sigue la misma tendencia que el agua recolectada mensual, y decrece con el promedio mensual de la amplitud diaria de la temperatura.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Fog water collection]]></kwd>
<kwd lng="en"><![CDATA[meteorology]]></kwd>
<kwd lng="en"><![CDATA[arid zones]]></kwd>
</kwd-group>
</article-meta>
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