<?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>S0187-62362024000100013</article-id>
<article-id pub-id-type="doi">10.20937/atm.53255</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Performance evaluation of the WRF model under different physical schemes for air quality purposes in Buenos Aires, Argentina]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Luque]]></surname>
<given-names><![CDATA[Solange E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fita]]></surname>
<given-names><![CDATA[Lluís]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pineda Rojas]]></surname>
<given-names><![CDATA[Andrea L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Buenos Aires Facultad de Ciencias Exactas y Naturales Centro de Investigaciones del Mar y la Atmósfera (CIMA), UBA-CONICET-CRNS-IRD IFAECI]]></institution>
<addr-line><![CDATA[Buenos Aires ]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>38</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362024000100013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362024000100013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362024000100013&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This work presents the performance evaluation of the Weather Research and Forecasting (WRF) model to estimate surface wind speed and direction, air temperature, and water vapor mixing ratio considering 22 configurations at high spatial resolution (1 km) during one week in winter and one week in spring, in order to determine the best-performing schemes for air quality purposes in the Metropolitan Area of Buenos Aires, Argentina. Results show that the use of urban schemes mostly affects wind speed and temperature. The single-layer urban canopy model (UCM) coupled with the Boulac planetary boundary layer (PBL) scheme exhibits the best results for wind speed. Wind direction and water vapor mixing ratio are more sensitive to the land surface model scheme, with results slightly improving with the Noah-MP land surface model. Wind speed and direction errors are larger when the former is lower. When removing from the analysis wind speed values below 2.6 m s-1 for the winter week and 3.1 m s-1 for the spring week, the root mean square errors for wind direction decreased between 50 and 72% of the original value, depending on the configuration and week. Overall, under the studied conditions, configurations including Noah-Mp land surface model or the combination of a simple UCM with BouLac PBL are suitable for air quality applications, as they reproduce both temperature and water vapor mixing ratio relatively well, with errors below 10% and Correlation values above 0.7, and are the best performing configurations for wind direction and speed, respectively.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Este trabajo presenta la evaluación de desempeño del Modelo para la Predicción e Investigación del Clima (WRF, por su sigla en inglés) para estimar la velocidad y dirección del viento, temperatura del aire y fracción de vapor de agua en superficie, considerando 22 configuraciones en alta resolución espacial (1 km) durante una semana de invierno y una de primavera, con el fin de determinar los esquemas que presentan mejor desempeño en el Área Metropolitana de Buenos Aires, Argentina, para ser utilizados en estudios de calidad del aire. Los resultados muestran que el uso de un esquema urbano afecta mayormente a la velocidad del viento y a la temperatura. El esquema urbano con una capa (UCM) acoplado con el esquema de capa límite (PBL) Boulac presenta el mejor desempeño para velocidad del viento. La dirección del viento y la fracción de vapor de agua son más sensibles al esquema de suelo, dando mejores resultados con el esquema de superficie Noah-Mp. Los errores tanto de dirección como de velocidad del viento son mayores cuando esta última toma valores pequeños. Al remover los valores de velocidad del viento menores a 2.6 m s-1 para la semana de invierno y 3.1 m s-1 para la de primavera, los errores cuadráticos de la dirección del viento decaen entre 50 y 72% de su valor original, dependiendo de la configuración y la semana. En general, en las condiciones estudiadas, las configuraciones que incluyen Noah-Mp o la combinación de Boulac con el esquema urbano simple son más adecuadas para utilizarse en estudios de calidad del aire, ya que reproducen de forma aceptable la temperatura y la fracción de vapor de agua con errores menores al 10% y Correlaciones mayores a 0.7, y poseen el mejor desempeño para dirección y velocidad del viento, respectivamente.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[WRF]]></kwd>
<kwd lng="en"><![CDATA[model evaluation]]></kwd>
<kwd lng="en"><![CDATA[sensitivity analysis]]></kwd>
<kwd lng="en"><![CDATA[urban scale]]></kwd>
</kwd-group>
</article-meta>
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