<?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>2664-0880</journal-id>
<journal-title><![CDATA[Revista Cubana de Meteorología]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Cubana Met.]]></abbrev-journal-title>
<issn>2664-0880</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Meteorológica de Cuba]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2664-08802020000100009</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis de la tormenta local severa ocurrida el 5 de mayo del 2018 en la provincia de Camagüey]]></article-title>
<article-title xml:lang="en"><![CDATA[Analysis of the severe local storm that occurred on May 5, 2018 in the province of Camagüey]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Estrada Canosa]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Navarro Silva]]></surname>
<given-names><![CDATA[Dainelaine]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bisbé Sifontes]]></surname>
<given-names><![CDATA[Luis Enrique]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro Meteorológico Provincial de Camagüey  ]]></institution>
<addr-line><![CDATA[ Camagüey]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2020</year>
</pub-date>
<volume>26</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S2664-08802020000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S2664-08802020000100009&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S2664-08802020000100009&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La presente investigación se basa en el estudio de una Tormenta Local Severa, ocurrida en la ciudad de Camagüey el 5 de Mayo del 2018, la cual estuvo relacionada con la presencia de una vaguada en superficie, reflejo de una baja fría superior en niveles medios de la tropósfera con presencia de corrientes del noreste y este, siendo la segunda condición de más influencia en nuestra provincia, que junto a fuerte calentamiento y el incremento de la energía hacen la combinación necesaria de la actividad convectiva y sobre todo a la caída de granizos y vientos linealmente fuerte los cuales pueden causar daños a la economía, la población, e incluso la pérdida de vidas humanas. En la investigación se presenta un análisis a partir del sondeo del horario de la 1800 UTC donde se analizaron los valores obtenidos de los principales índices termodinámicos como la energía convectiva potencial disponible (CAPE), índice de levantamiento (LI), índice total totales (TT), total cruzado (TC), índice Kaidach (KI) y el índice de amenaza de tiempo severo (SWEAT). Se analiza el comportamiento medio de la humedad en la capa de superficie a 3 y 6 km respectivamente, así como la estructura vertical del viento, caracterizada por los niveles de 850, 700, 600 y 500 hPa. El resultado que se expone puede servir de guía durante el desarrollo del trabajo operativo de los meteorólogos en la vigilancia meteorológica.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The present investigation is based on the study of a Severe Local Storm, which occurred in the city of Camagüey on May 5, 2018, which was related to the presence of a surface trough, reflecting a higher cold fall in average levels of the troposphere with the presence of currents from the northeast and east, being the second most influential condition in our province, which together with strong warming and increased energy make the necessary combination of convective activity and especially the fall of hail and linearly strong winds which can cause damage to the economy, the population, and even the loss of human lives. The investigation presents an analysis based on the survey of the 1800 UTC schedule where the values &#8203;&#8203;obtained from the main thermodynamic indices were analyzed, such as the potential convective energy available (CAPE), the survey index (LI), total total index (TT), crossed total (TC), Kaidach index (KI) and the severe weather threat index (SWEAT). The average behavior of the humidity in the surface layer at 3 and 6 km respectively is analyzed, as well as the vertical structure of the wind, characterized by the levels of 850, 700, 600 and 500 hPa. The result that is exposed can serve as a guide during the development of meteorologists' operational work in meteorological surveillance.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Tormenta local severa]]></kwd>
<kwd lng="es"><![CDATA[Sondeo aerológico]]></kwd>
<kwd lng="en"><![CDATA[Local severe storm]]></kwd>
<kwd lng="en"><![CDATA[Sound aerologic]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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