<?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>S0187-62362021000100111</article-id>
<article-id pub-id-type="doi">10.20937/atm.52680</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Parametric study of hurricanes intensity as they move over land]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pastrana]]></surname>
<given-names><![CDATA[Daniel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Treviño]]></surname>
<given-names><![CDATA[César]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Ingeniería Laboratorio de Ingeniería y Procesos Costeros]]></institution>
<addr-line><![CDATA[Sisal Yucatán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ciencias Unidad Multidisciplinaria en Docencia e Investigación Sisal]]></institution>
<addr-line><![CDATA[Sisal Yucatán]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>34</volume>
<numero>1</numero>
<fpage>111</fpage>
<lpage>120</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362021000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362021000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362021000100111&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Two of the most important tropical cyclone parameters, which are used as a measure of their intensity, are the maximum surface wind speed (local parameter) and the pressure difference between the free atmosphere and the pressure in the center of the storm (global parameter). In this paper we reexamined the relationship between these parameters via the Euler number, which is a nondimensional parameter that relates the overall pressure difference to the dynamic pressure generated by the maximum value of the wind speed. The calculations were performed all along the track of 20 tropical cyclones using the National Hurricane Center&#8217;s extended best track database for the Atlantic basin. It was found that when the cyclone is over water, the Euler number tends to remain constant, while over land the parameter varies drastically with a tendency to grow. These results confirm that over sea, when they have reached hurricane strength, tropical cyclones evolve slowly remaining near the steady state, highlighting the importance of transient states during strong dissipation. The Euler number seems to be independent of the global warming.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Dos de los parámetros más importantes del ciclón tropical, que se utilizan como una medida de su intensidad, son la velocidad máxima del viento en la superficie (parámetro local) y la diferencia de presión entre la atmósfera libre y la presión en el centro de la tormenta (parámetro global). En este documento reexaminamos la relación entre estos parámetros a través del número de Euler. El número de Euler es un parámetro adimensional que relaciona la diferencia de presión global con la presión dinámica generada por el valor máximo de la velocidad del viento. Los cálculos se realizaron a lo largo del recorrido de veinte ciclones tropicales utilizando la base de datos del Centro Nacional de Huracanes de EUA para la cuenca del Atlántico. Se encontró que cuando el ciclón está sobre el agua, el número de Euler tiende a permanecer constante, mientras que sobre tierra el parámetro varía drásticamente con una tendencia a crecer, confirmando que en el mar, cuando ha alcanzado la intensidad de huracán, los ciclones tropicales evolucionan lentamente permaneciendo cerca del estado estacionario, resaltando la importancia de los efectos transitorios al tocar tierra la tormenta. El número de Euler en ciclones tropicales es independiente del calentamiento global.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[tropical hurricanes]]></kwd>
<kwd lng="en"><![CDATA[storm intensity]]></kwd>
<kwd lng="en"><![CDATA[Euler number]]></kwd>
<kwd lng="en"><![CDATA[minimal storm pressure]]></kwd>
<kwd lng="en"><![CDATA[landfalling effects]]></kwd>
</kwd-group>
</article-meta>
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