<?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>S0187-62362022000100111</article-id>
<article-id pub-id-type="doi">10.20937/atm.52900</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Wind profile analysis for selected tropical cyclones over the South China Sea based on dropsonde measurements]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[He]]></surname>
<given-names><![CDATA[J. Y.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hon]]></surname>
<given-names><![CDATA[K. K.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Li]]></surname>
<given-names><![CDATA[Q. S.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Chan]]></surname>
<given-names><![CDATA[P. W.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,City University of Hong Kong Department of Architecture and Civil Engineering ]]></institution>
<addr-line><![CDATA[Hong Kong ]]></addr-line>
<country>China</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Hong Kong Observatory  ]]></institution>
<addr-line><![CDATA[Kowloon Hong Kong]]></addr-line>
<country>China</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>111</fpage>
<lpage>126</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-62362022000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-62362022000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-62362022000100111&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Vertical wind profiles of selected tropical cyclones over the South China Sea are studied for the first time using dropsonde measurements by a fixed-wing aircraft of the Hong Kong Government. They are studied in two aspects which have not been conducted before for storms over the South China Sea. First the strengthening and weakening of the tropical cyclones are analyzed based on the radial wind profiles, namely, inflow and outflow, particularly over the atmospheric boundary layer. Second, the vertical wind profiles are fitted using the commonly considered wind profile models reported in the literature and compared with stipulations in Hong Kong and Chinese structural design codes. This would have significant contributions to wind engineering applications in the region. The results are unique for tropical cyclones over South China Sea and would serve as useful reference for the studies of tropical cyclones in this ocean basin.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Se estudian por primera vez los perfiles verticales del viento de algunos ciclones tropicales del mar de China Meridional, utilizando para ello mediciones de radiosondas lanzadas desde una aeronave del gobierno de Hong Kong. Se analizan dos aspectos de dichos perfiles relativos a tormentas en el mar de China Meridional, los cuales no se han abordado antes. Primero, se estudian el fortalecimiento y el debilitamiento de los ciclones tropicales con base en perfiles radiales del viento, específicamente de entrada y de salida, en particular sobre la capa límite atmosférica. En segundo lugar, se ajustan los perfiles verticales del viento utilizando para ello los modelos de perfiles de viento más reportados en la literatura y se les compara con las especificaciones de las normas chinas y hongkonesas para el diseño de estructuras, lo cual constituye una importante contribución a las aplicaciones de ingeniería de vientos en la región. Los resultados son exclusivos para ciclones tropicales en el mar de China Meridional y pueden servir como referencia útil para su estudio en esa cuenca oceánica.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[dropsonde]]></kwd>
<kwd lng="en"><![CDATA[tropical cyclone]]></kwd>
<kwd lng="en"><![CDATA[vertical wind profile for wind engineering application]]></kwd>
</kwd-group>
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