<?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>2007-2422</journal-id>
<journal-title><![CDATA[Tecnología y ciencias del agua]]></journal-title>
<abbrev-journal-title><![CDATA[Tecnol. cienc. agua]]></abbrev-journal-title>
<issn>2007-2422</issn>
<publisher>
<publisher-name><![CDATA[Instituto Mexicano de Tecnología del Agua, Coordinación de Comunicación, Participación e Información]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-24222021000400421</article-id>
<article-id pub-id-type="doi">10.24850/j-tyca-2021-04-10</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Determinación del coeficiente de avance de la tormenta según el origen y peligro de las precipitaciones en el archipiélago cubano]]></article-title>
<article-title xml:lang="en"><![CDATA[Storm advancement coefficient determination according to origin and hazard rainfall in the Cuban archipelago]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-González]]></surname>
<given-names><![CDATA[Yoel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Planos-Gutiérrez]]></surname>
<given-names><![CDATA[Eduardo O.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de La Habana Instituto Superior de Tecnología y Ciencias Aplicadas ]]></institution>
<addr-line><![CDATA[La Habana ]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto de Meteorología Centro del Clima ]]></institution>
<addr-line><![CDATA[La Habana ]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2021</year>
</pub-date>
<volume>12</volume>
<numero>4</numero>
<fpage>421</fpage>
<lpage>450</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-24222021000400421&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-24222021000400421&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-24222021000400421&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En este trabajo se presenta una generalización de la metodología de Martínez, Planos y Perdigón (2020), y se determina el coeficiente de avance de las tormentas y su relación con el hietograma de precipitación de tormentas de tipo específico. El coeficiente de avance de la tormenta es un parámetro hidrológico utilizado por muchos autores para determinar el instante donde tiene lugar la intensidad máxima de la precipitación. Esto facilita la selección del modelo de distribución temporal de precipitaciones, criterio de gran utilidad para el diseño de obras de ingeniería y la predicción hidrológica. En este artículo se aborda el tema definiendo el coeficiente de avance según el origen y peligrosidad de la precipitación, fundamentalmente para las precipitaciones causadas por los eventos meteorológicos propios de la interacción trópico-latitudes medias, tropicales no ciclónicos y ciclónicos. Entre los resultados figura la obtención de los hietogramas de precipitación para diferentes sistemas meteorológicos, así como diversos tipos de peligrosidad, lo cual le otorga carácter climático y regional. El área de estudio abarca todo el territorio cubano.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In this paper, a generalization methodology of Martínez, Planos and Perdigón (2020) is presented. The storm advancement coefficient and its relationship with the specific type of storm precipitation hyetograph is determined. The storm advancement coefficient is a hydrological parameter used to determine the instant where the maximum rainfall intensity occurs for specific storms. This issue the selection of the rainfall temporal distribution model, which is very useful for hydraulic engineering design and hydrological prediction. The proposed approach, define the coefficient according to rainfall origin and its hazard; mainly for the meteorological events typical of the tropic interaction-middle latitudes, non-cyclonic tropical, and cyclonic. Finally, rainfall hyetographs for different hydrometeorological systems were obtained, as well as several types of hazards, which gives it a climatic and regional character. This paper is for the entire Cuban territory.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[precipitaciones]]></kwd>
<kwd lng="es"><![CDATA[coeficiente de avance de la tormenta]]></kwd>
<kwd lng="es"><![CDATA[peligro]]></kwd>
<kwd lng="es"><![CDATA[curvas IDF]]></kwd>
<kwd lng="en"><![CDATA[Rainfalls]]></kwd>
<kwd lng="en"><![CDATA[storm advancement coefficient]]></kwd>
<kwd lng="en"><![CDATA[hazard]]></kwd>
<kwd lng="en"><![CDATA[IDF curves]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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