<?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>0430-5027</journal-id>
<journal-title><![CDATA[Finisterra - Revista Portuguesa de Geografia]]></journal-title>
<abbrev-journal-title><![CDATA[Finisterra]]></abbrev-journal-title>
<issn>0430-5027</issn>
<publisher>
<publisher-name><![CDATA[Centro de Estudos Geográficos]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0430-50272022000200129</article-id>
<article-id pub-id-type="doi">10.18055/finis24940</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Inversiones térmicas nocturnas con estrato cálido en niveles atmosféricos bajos: contrastes térmicos significativos en la Demarcación Hidrográfica del Segura (2011-2020).]]></article-title>
<article-title xml:lang="pt"><![CDATA[Inversões térmicas noturnas com estrato quente nos níveis baixos da atmosfera: contrastes térmicos significativos na Demarcação Hidrográfica do Rio Segura (2011-2020).]]></article-title>
<article-title xml:lang="en"><![CDATA[Nocturnal temperature inversions with warm layer at low atmospheric levels: significant thermal contrasts in the Segura River Basin District (2011-2020).]]></article-title>
<article-title xml:lang="fr"><![CDATA[Inversions thermiques nocturnes à strate chaude dans les bas niveaux atmosphériques: contrastes thermiques importants dans le District Hydrographique du Bassin du Fleuve Segura (2011-2020).]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sanchez]]></surname>
<given-names><![CDATA[David Espín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Murcia Facultad de Letras Departamento de Geografía]]></institution>
<addr-line><![CDATA[Murcia ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>30</day>
<month>08</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>30</day>
<month>08</month>
<year>2022</year>
</pub-date>
<numero>120</numero>
<fpage>129</fpage>
<lpage>156</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_arttext&amp;pid=S0430-50272022000200129&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_abstract&amp;pid=S0430-50272022000200129&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_pdf&amp;pid=S0430-50272022000200129&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El sureste de la península ibérica (España) se caracteriza por una importante recurrencia temporal de los procesos de inversión térmica nocturna (ITN), debido principalmente a la gran cantidad de días despejados a lo largo del año. La Demarcación Hidrográfica del Segura (DHS) posee desnivel altitudinal de 2100m en 150km, con alternancia de zonas de valle y espacios orográficamente complejos y accidentados. Ello da lugar a marcados contrastes térmicos nocturnos, cuyas diferencias térmicas verticales se sitúan en 13,0ºC entre zonas de piscinas de aire frío o cold air pools (CAP) y superficies orográficamente accidentadas. Se analizan los contrastes térmicos a través de 58 observatorios meteorológicos en las 50 madrugadas con la mayor intensidad de inversión térmica en los últimos años de observación (2011-2020). Se analiza, además, las características y causas desencadenantes de tales procesos, a través del análisis de variables influyentes en la distribución de temperaturas mínimas (viento, humedad relativa, &#8230;). Además, se presenta una técnica de análisis satelital de alta resolución, a través de la elaboración de termografías (distribución de temperaturas superficiales) mediante el sensor ASTER, que vienen a complementar, desde el punto de vista espacial, la distribución de temperaturas mínimas en madrugadas de ITN en algunos sectores del área de estudio. Entre los resultados más concluyentes destacan notables diferencias térmicas durante las madrugadas estables (diferencias medias de 7,1ºC y absolutas de 13ºC entre observatorios situados en fondos de valle (CAP) y aquellos ubicados a mayor altitud, en zonas orográficamente accidentadas), registradas bajo masas de aire templadas y secas a un nivel geopotencial de 850 hPa.]]></p></abstract>
<abstract abstract-type="short" xml:lang="pt"><p><![CDATA[Resumo O sudeste da península ibérica (Espanha) caracteriza-se por uma importante recorrência temporal de processos noturnos de inversão térmica (ITN), principalmente devido ao grande número de dias de céu limpo ao longo do ano. A região hidrográfica do Rio Segura (DHS) tem uma diferença de altitude de 2100m em 150km, com áreas de vale que alternam com áreas orograficamente complexas e acidentadas. Isto dá origem a contrastes térmicos noturnos marcados, cujas diferenças térmicas verticais são de 13,0ºC entre áreas de lagos de ar frio ou cold air pools (CAP) e superfícies irregulares. Os contrastes térmicos são analisados através de 58 observatórios meteorológicos nas 50 manhãs com maior intensidade de inversão térmica nos últimos anos de observação (2011-2020). As características e as causas desencadeantes desses processos são analisadas através da análise de variáveis que influenciam a distribuição das temperaturas mínimas (vento, humidade relativa, ...). Além disso, é apresentada uma técnica de análise de satélite de alta resolução, através da elaboração de termografias (distribuição de temperaturas de superfície) por meio do sensor ASTER, que complementam, do ponto de vista espacial, a distribuição de temperaturas mínimas nas primeiras horas das manhãs de ITN em alguns setores da área de estudo. Entre os resultados mais conclusivos, destacam-se diferenças térmicas notáveis durante madrugadas estáveis (diferenças médias de 7,1ºC e diferenças absolutas de 13ºC entre observatórios localizados em fundos de vales (CAP) e aqueles localizados em altitudes mais elevadas, em áreas orograficamente acidentadas), sob a influência de massas de ar quente e seco a um nível geopotencial de 850hPa.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The southeast of the Iberian Peninsula (Spain) is characterized by a significant recurrence of nocturnal temperature inversion processes (ITN), mainly due to the large number of clear days throughout the year. The Segura River Basin District (DHS) has an altitude difference of 2100m in 150km with alternating valley areas and orographically complex and rugged areas. This gives rise to marked night-time thermal contrasts, whose vertical thermal differences are 13.0ºC between cold air pools (CAP) and more prominent surfaces. Thermal contrasts are analysed through 58 meteorological observatories in the 50 mornings with the highest intensity of thermal inversion in the last years of observation (2011-2020). Furthermore, the characteristics and triggering causes of such processes are analysed through the analysis of variables influencing the distribution of minimum temperatures (wind, relative humidity, ...). In addition, a high-resolution satellite analysis technique is presented, through the elaboration of thermographies (distribution of surface temperatures) by means of the ASTER sensor, which complement, from the spatial point of view, the distribution of minimum temperatures in the early mornings of ITN in some sectors of the study area. Among the most conclusive results, notable thermal differences stand out during stable early mornings (mean differences of 7.1ºC and absolute differences of 13ºC between observatories located at valley bottoms (CAP) and those located at higher altitudes, in orographically rugged areas), recorded under warm and dry air masses at a geopotential level of 850hPa.]]></p></abstract>
<abstract abstract-type="short" xml:lang="fr"><p><![CDATA[Résumé Le sud-est de la péninsule ibérique (Espagne) est caractérisé par une récurrence importante des processus d&#8217;inversion thermique nocturne (ITN), principalement en raison du grand nombre de jours clairs tout au long de l&#8217;année. Le district du bassin du fleuve Segura (DHS) a une différence d&#8217;altitude de 2100m en 150km, avec des zones de vallées alternées et des zones orographiquement complexes et accidentées. Il en résulte des contrastes thermiques nocturnes marqués, dont les différences thermiques verticales sont de 13,0ºC entre les zones de bassins d&#8217;air froid ou bassins d&#8217;air froid (PAC) et les surfaces irrégulières. Les contrastes thermiques sont analysés à travers 58 observatoires météorologiques au cours des 50 matinées avec la plus forte intensité d&#8217;inversion thermique au cours des dernières années d&#8217;observation (2011-2020). Par ailleurs, les caractéristiques et les causes de déclenchement de tels processus sont analysées à travers l&#8217;analyse de variables qui influencent la répartition des températures minimales (vent, humidité relative, ...). De plus, une technique d&#8217;analyse satellitaire à haute résolution (au moyen du sensor ASTER) est présentée, à travers l&#8217;élaboration de thermographies (distribution des températures de surface), qui complètent, du point de vue spatial, la distribution des températures minimales au petit matin de NTI dans certains secteurs de la zone d&#8217;étude. Parmi les résultats les plus concluants, des différences thermiques notables se distinguent lors de matinées stables (différences moyennes de 7,1°C et différences absolues de 13°C entre les observatoires situés au fond des vallées (CAP) et ceux situés à des altitudes plus élevées, dans des zones orographiquement accidentées), enregistrées sous masses d&#8217;air chaud et sec à un niveau géo-potentiel de 850hPa.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Inversión térmica]]></kwd>
<kwd lng="es"><![CDATA[viento]]></kwd>
<kwd lng="es"><![CDATA[humedad]]></kwd>
<kwd lng="es"><![CDATA[termografía]]></kwd>
<kwd lng="es"><![CDATA[distribución]]></kwd>
<kwd lng="pt"><![CDATA[Inversão térmica]]></kwd>
<kwd lng="pt"><![CDATA[vento]]></kwd>
<kwd lng="pt"><![CDATA[humidade]]></kwd>
<kwd lng="pt"><![CDATA[termografia]]></kwd>
<kwd lng="pt"><![CDATA[distribuição]]></kwd>
<kwd lng="en"><![CDATA[Thermal inversion]]></kwd>
<kwd lng="en"><![CDATA[wind]]></kwd>
<kwd lng="en"><![CDATA[humidity]]></kwd>
<kwd lng="en"><![CDATA[thermography]]></kwd>
<kwd lng="en"><![CDATA[distribution]]></kwd>
<kwd lng="fr"><![CDATA[Inversion thermique]]></kwd>
<kwd lng="fr"><![CDATA[vent]]></kwd>
<kwd lng="fr"><![CDATA[humidité]]></kwd>
<kwd lng="fr"><![CDATA[thermographie]]></kwd>
<kwd lng="fr"><![CDATA[distribution]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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