<?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>1680-0338</journal-id>
<journal-title><![CDATA[Ingeniería Hidráulica y Ambiental]]></journal-title>
<abbrev-journal-title><![CDATA[riha]]></abbrev-journal-title>
<issn>1680-0338</issn>
<publisher>
<publisher-name><![CDATA[Centro de Investigaciones Hidráulicas (CIH). Facultad de Ingeniería Civil. Universidad Tecnológica de La Habana "José A. Hecheverría" CUJAE]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1680-03382020000200003</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Hidrodinámica costera durante el huracán Wilma (2005) en Artemisa, Mayabeque y La Habana]]></article-title>
<article-title xml:lang="en"><![CDATA[Coastal hydrodynamics during Hurricane Wilma (2005) in Artemisa, Mayabeque and Havana]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez Pérez]]></surname>
<given-names><![CDATA[Janner]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Córdova López]]></surname>
<given-names><![CDATA[Luis F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Díaz García]]></surname>
<given-names><![CDATA[Ovel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Ciego de Ávila  ]]></institution>
<addr-line><![CDATA[ Ciego de Ávila]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Tecnológica de La Habana José Antonio Echeverría (CUJAE)  ]]></institution>
<addr-line><![CDATA[ La Habana]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Ciencias de la Atmósfera ]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2020</year>
</pub-date>
<volume>41</volume>
<numero>2</numero>
<fpage>3</fpage>
<lpage>17</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S1680-03382020000200003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S1680-03382020000200003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S1680-03382020000200003&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Este trabajo tuvo como objetivo estudiar, mediante simulación computacional, la influencia sobre el nivel del mar de los fenómenos: marea astronómica, surgencia y oleaje en las costas de las provincias Artemisa, Mayabeque y La Habana. Los códigos ADCIRC y ADCIRC+SWAN fueron ejecutados en tres escenarios, forzados por componentes de la marea y forzadores atmosféricos. Se seleccionó el huracán Wilma (2005). Se definieron ocho localidades: cuatro en la costa norte y cuatro al sur de la zona de estudio. Los resultados se comparan con datos aportados por la NOAA. Se concluyó que la surgencia de tormenta fue el fenómeno que más elevación del mar produjo en los sitios de la costa sur, mientras al norte la marea astronómica reportó los mayores niveles.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This work aimed to study, through computer simulation, the influence on sea level of the following phenomena: astronomical tide, storm surge and waves on the coasts of the provinces Artemisa, Mayabeque and Havana. The ADCIRC and ADCIRC + SWAN codes were executed in three scenarios, forced by components of the tide and atmospheric forces. Hurricane Wilma (2005) was selected. Eight locations were defined: four on the north coast and four south of the study area. The results are compared with data provided by NOAA. It was concluded that the storm surge was the phenomenon that increased more the sea level in the sites of the southern coast, while in the northern coast the astronomical tide reported the highest levels.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[hidrodinámica]]></kwd>
<kwd lng="es"><![CDATA[huracanes]]></kwd>
<kwd lng="es"><![CDATA[modelación numérica]]></kwd>
<kwd lng="es"><![CDATA[surgencia]]></kwd>
<kwd lng="en"><![CDATA[hydrodynamics]]></kwd>
<kwd lng="en"><![CDATA[hurricanes]]></kwd>
<kwd lng="en"><![CDATA[numerical modeling]]></kwd>
<kwd lng="en"><![CDATA[storm surge]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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