<?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>S0187-62362023000300113</article-id>
<article-id pub-id-type="doi">10.20937/atm.53039</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The planetary boundary layer physical processes, the secondary thermal baroclinic circulation and inertial oscillation contribution to diurnal variation of the Etesian winds over the Aegean Sea]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Prezerakos]]></surname>
<given-names><![CDATA[Nicholas G.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,University of West Attica Emeritus Professor, School of Engineering ]]></institution>
<addr-line><![CDATA[Attica ]]></addr-line>
<country>Greece</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>37</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362023000300113&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362023000300113&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362023000300113&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Etesian winds constitute an important climatological phenomenon, which does not only moderate the heat during the summer in the Aegean Sea, but provides a source of clean renewable energy as well. Even though several papers have attempted to explain their dynamical and physical characteristics, the respective processes that drive the diurnal variation of the wind speed are not fully understood. The objective of this paper is to identify the processes responsible for diurnal variation with observed maximum wind speed around noon and minimum around midnight. Analytical solutions of a primitive equation set in Eulerian form, after introducing suitable conditions and approximations, reveal an inertial oscillation over the Aegean Sea. Data based on direct observations, ECMWF IFS high resolution analyses and high-resolution simulations with the Weather Research and Forecasting (WRF) model are utilized to find out the type and structure of the planetary boundary layer (PBL) over the Aegean Sea. This PBL appears to be of a marine character and turbulent mostly during the day but less during the night. The direct impact of local and regional thermally-driven circulations is found to be the main cause of the diurnal variation of the observed wind and partly the inertial oscillation. Results from numerical simulations certify these findings. Furthermore, the momentum and Newtonian heating exchanges by the physical processes inside the PBL, where the gradient wind together with smaller scales of atmospheric motions exist, are also necessary for explaining the variability of the Etesian winds.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los vientos etesianos constituyen un fenómeno climatológico importante, que no sólo modera el calor durante el verano en el mar Egeo, sino que también proporciona una fuente de energía renovable limpia. A pesar de que varios artículos han intentado explicar sus características dinámicas y físicas, los procesos respectivos que impulsan la variación diurna de la velocidad del viento no se entienden completamente. El objetivo de este trabajo es identificar los procesos responsables de la variación diurna con la velocidad máxima del viento observada alrededor del mediodía y la mínima alrededor de la medianoche. Las soluciones analíticas de una ecuación primitiva establecida en forma euleriana, después de introducir condiciones y aproximaciones adecuadas, revelan una oscilación inercial sobre el mar Egeo. Los datos basados en observaciones directas, los análisis de alta resolución ECMWF IFS y las simulaciones de alta resolución con el modelo Investigación y Pronóstico del Clima (WRF, por sus siglas en inglés) se utilizan para averiguar el tipo y la estructura de la capa límite planetaria (PBL) sobre el mar Egeo. Esta PBL parece ser de carácter marino y turbulento, principalmente durante el día y menos durante la noche. Se ha encontrado que el impacto directo de las circulaciones locales y regionales impulsadas térmicamente es la causa principal de la variación diurna del viento observado y en parte de la oscilación inercial. Los resultados de las simulaciones numéricas certifican estos hallazgos. Además, el momento y los intercambios de calentamiento newtonianos por los procesos físicos dentro de la PBL, donde está presente el viento de gradiente junto con escalas más pequeñas de movimientos atmosféricos, también son necesarios para explicar la variabilidad de los vientos etesianos.]]></p></abstract>
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<kwd lng="en"><![CDATA[planetary boundary layer structure]]></kwd>
<kwd lng="en"><![CDATA[Eulerian equations of inertial oscillation]]></kwd>
<kwd lng="en"><![CDATA[planetary boundary layer momentum moisture and heat transfer]]></kwd>
<kwd lng="en"><![CDATA[local and regional sea and mountain breezes]]></kwd>
<kwd lng="en"><![CDATA[high resolution analyses and simulations]]></kwd>
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</article-meta>
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