<?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>S0187-62362022000100089</article-id>
<article-id pub-id-type="doi">10.20937/atm.52838</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Etesian winds outbursts over the Greek Seas and their linkage with larger-scale atmospheric circulation features: Two real time data case studies]]></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 School of Engineering ]]></institution>
<addr-line><![CDATA[Athens ]]></addr-line>
<country>Greece</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>35</volume>
<numero>1</numero>
<fpage>89</fpage>
<lpage>110</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362022000100089&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362022000100089&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362022000100089&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT There are significant differences in the way that researchers have defined &#8220;Etesian wind days&#8221;. An attempt is made here to establish common definitions of the various types of Etesian winds from the weather forecaster&#8217;s viewpoint. These definitions are based on objective criteria adopted from the frequency of atmospheric circulation features associated with the occurrence of the Etesian winds and their physical characteristics. The presence of fairly constant northerly winds over the Greek Seas in summer are called Etesian winds. When a new spell of Etesian winds is established with no diurnal variation of the wind direction for consecutive days (maximum of seven), these winds are called &#8220;type B&#8221; Etesian winds or &#8220;Etesian outbursts&#8221;. The atmospheric circulations associated with the occurrence, origin and evolution of the type B Etesian winds and the accompanying weather are revealed utilizing data for the period 1975-2015 and focusing on two case studies on July 21-22, 1983 and July 3-4, 2017. The presence of the Subtropical Jet Stream (SJS) over the Greek territory and its interaction with the Polar Jet Stream (PJS) are dominant factors. Large-scale atmospheric circulations are studied to identify simultaneous direct links to the Indian Summer Monsoon (ISM), El Niño-Southern Oscillation (ENSO), Madden-Julian Oscillation (JMO), deep convective activity in the Hadley circulation in the tropics, and West Africa Monsoon (WAM).]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Hay diferencias significativas entre las formas en que los investigadores han definido el término «días de etesios». El presente trabajo intenta establecer definiciones comunes para varios vientos de este tipo desde el punto de vista meteorológico. Estas definiciones se basan en criterios objetivos basados en la frecuencia con que se presentan ciertas características de la circulación asociadas con la ocurrencia de dichos vientos. Se denomina etesios a los vientos constantes del norte cuya presencia en los mares de Grecia durante el verano es bastante frecuente. Cuando se instaura una nueva racha de etesios sin variación diurna de la dirección del viento por varios días consecutivos (con un máximo de siete) se les denomina etesios de «tipo B» o «racha de etesios». Se utilizan datos del periodo 1975-2015 y dos casos de estudio (21-22 de julio de 1983 y 3-4 de julio de 2017) para analizar los tipos de circulación atmosférica asociados con la ocurrencia, origen y evolución de este fenómeno, así como el tiempo meteorológico concomitante. La presencia de una corriente en chorro subtropical sobre el territorio griego y su interacción con la corriente en chorro polar constituyen factores dominantes. Se estudian las circulaciones atmosféricas de larga escala para identificar conexiones directas con el monzón de verano de la India, El Niño-Oscilación del Sur, la oscilación Madden-Julian, actividad conectiva profunda en la circulación tropical de Hadley y el monzón de África Occidental.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Etesian wind days]]></kwd>
<kwd lng="en"><![CDATA[Polar Jet stream]]></kwd>
<kwd lng="en"><![CDATA[Indian Summer Monsoon]]></kwd>
<kwd lng="en"><![CDATA[West African Monsoon]]></kwd>
</kwd-group>
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