<?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>S0430-50272021000300025</article-id>
<article-id pub-id-type="doi">10.18055/finis21158</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Climate variability and anthropogenic actions as drivers for aeolian activity during the last millennium in south-western Europe: A case study on the portuguese coast]]></article-title>
<article-title xml:lang="pt"><![CDATA[Variabilidade climática e ações antrópicas como impulsionadores da atividade eólica durante o último milénio no sudoeste da Europa. Um caso de estudo da costa portuguesa]]></article-title>
<article-title xml:lang="fr"><![CDATA[La variabilité climatique et les actions anthropiques comme declencheurs de l&#8217;activité éolienne au cours du dernier millénaire en sud-oest de l&#8217;Europe. Une étude de cas sur la côte portugaise]]></article-title>
<article-title xml:lang="es"><![CDATA[La variabilidad climática y las acciones antrópicas como impulsores de la actividad eólica durante el último milenio en el sudoeste de Europa: un estudio de caso de la costa protuguesa]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tudor]]></surname>
<given-names><![CDATA[Mihaela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
<xref ref-type="aff" rid="A a"/>
<xref ref-type="aff" rid="A3"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ramos-Pereira]]></surname>
<given-names><![CDATA[Ana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Freitas]]></surname>
<given-names><![CDATA[Joana Gaspar de]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidade de Lisboa Centro de História, Faculdade de Letras ]]></institution>
<addr-line><![CDATA[Lisboa ]]></addr-line>
<country>Portugal</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidade de Lisboa Instituto de Geografia e Ordenamento do Território Centro de Estudos Geográficos]]></institution>
<addr-line><![CDATA[Lisboa ]]></addr-line>
<country>Portugal</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidade de Lisboa Instituto de Geografia e Ordenamento do Território Laboratório Associado TERRA]]></institution>
<addr-line><![CDATA[Lisboa ]]></addr-line>
<country>Portugal</country>
</aff>
<pub-date pub-type="pub">
<day>30</day>
<month>12</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>30</day>
<month>12</month>
<year>2021</year>
</pub-date>
<numero>118</numero>
<fpage>25</fpage>
<lpage>51</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_arttext&amp;pid=S0430-50272021000300025&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_abstract&amp;pid=S0430-50272021000300025&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.pt/scielo.php?script=sci_pdf&amp;pid=S0430-50272021000300025&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The building of dunes and sand drifts along the European coastline are generally related to climatic variability and sea-level fluctuation. The last phase of dunes formation in south-western Europe coincides with the Little Ice Age (LIA) period characterized by pronounced climate variability. Historical sources retrieved from archives also report sand-drift events along the Portuguese coast. The sand invaded many agricultural fields, and settlements, forcing the inhabitants to move elsewhere. The article explores the temporal relationships between sand drift occurrences and climate, as a principal trigger for coastal dune migration. We used historical sources about sand-drift events as documentary proxies to infer the past climate variability on the Portuguese coast. Three spatial scales of climate variability were considered: i) the global climatic variability induced by the cold abrupt events over the last Millennium (LIA); ii) the regional (mesoscale) climate variability (NAO index), and iii) the local climate variability (extreme meteorological events). The paleoclimatic interpretation indicates that drifts in Portugal are related to both NAO modes, providing new insights into coastal dunes dynamics, as a response to natural drivers. However, the analysis of human activity on the coast also allowed us to better understand the relation of the local populations with their environments, highlighting those anthropogenic actions caused an additional disturbance on coastal dune dynamics.]]></p></abstract>
<abstract abstract-type="short" xml:lang="pt"><p><![CDATA[Resumo A construção de dunas e os movimentos de areia ao longo da costa europeia estão geralmente relacionados com a variabilidade climática e com a flutuação do nível do mar. A última fase da formação de dunas no sudoeste da Europa coincide com o período da Pequena Idade do Gelo (LIA), caracterizado por uma pronunciada variabilidade climática. Fontes históricas extraídas de arquivos referem ocorrências de invasão de areia ao longo da costa portuguesa. A areia invadiu muitos campos agrícolas e povoações, forçando os habitantes a mudarem-se para outros lugares. O artigo explora as relações temporais entre as ocorrências de invasão das areias dunares devido ao vento e o clima, como principal impulsionador para a migração das dunas costeiras. Foram utilizadas fontes históricas sobre eventos de deriva de areia como proxies documentais para inferir a variabilidade climática passada na costa portuguesa. Três escalas espaciais de variabilidade climática foram consideradas: i) a variabilidade climática global induzida pelos eventos abruptos frios ao longo do último milénio (LIA); ii) a variabilidade climática regional (de mesoescala - índice NAO); e iii) a variabilidade do clima local (eventos meteorológicos extremos). A interpretação paleoclimática indica que os movimentos de areia em Portugal estão relacionados com ambos os modos do índice NAO, proporcionando novos conhecimentos sobre a dinâmica das dunas costeiras, em resposta às condicionantes naturais. No entanto, a avaliação da atividade humana no litoral também nos permitiu compreender melhor a relação das populações locais com os seus ambientes, destacando que as ações antrópicas causaram um distúrbio adicional na dinâmica das dunas costeiras.]]></p></abstract>
<abstract abstract-type="short" xml:lang="fr"><p><![CDATA[Résumé La formation de dunes et les dérives de sable le long du littoral européen sont généralement liées à la variabilité climatique et aux fluctuations du niveau de la mer. La dernière phase de formation des dunes dans le sud-ouest de l&#8217;Europe coïncide avec la période du Petit Âge Glaciaire (LIA) caractérisée par une variabilité climatique. Les sources historiques extraites du rapport d&#8217;archives mettent en évidence des occurrences de dérive de sable le long de la côte portugaise. Le sable a envahi de nombreux champs et établissements agricoles, obligeant les habitants à se déplacer ailleurs. L&#8217;article explore les relations temporelles entre les événements de dérives de sable à cause du vent et le climat comme principal déclencheur de la migration des dunes côtières. Nous avons utilisé des sources historiques sur les événements de dérive de sable comme substituts documentaires pour déduire la variabilité climatique passée dans la côte portugaise. Trois échelles spatiales de variabilité climatique ont été considérées : i) la variabilité climatique globale induite par les événements froids brusques au cours du dernier millénaire (LIA) ; ii) la variabilité climatique régionale (méso-échelle) (indice NAO) ; et iii) la variabilité du climat local (par exemple les événements météorologiques extrêmes). L&#8217;interprétation paléoclimatique indique que les dérives de sable au Portugal sont liées aux deux modes NAO, offrant de nouvelles perspectives sur la dynamique des dunes côtières, en réponse aux facteurs naturels. Cependant, l&#8217;analyse de l&#8217;activité humaine le long du littoral a également permis de mieux comprendre la relation des populations locales avec leur environnement, soulignant que les actions anthropiques ont provoqué une perturbation supplémentaire sur la dynamique des dunes côtières.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La construcción de dunas y los movimientos de arena a lo largo de la costa europea están generalmente relacionados con la variabilidad climática y la fluctuación del nivel del mar. La última fase de formación de dunas en el suroeste de Europa coincide con el período de la Pequeña Edad de Hielo (LIA), caracterizado por una pronunciada variabilidad climática. Las fuentes históricas extraídas de archivos se refieren a eventos de movimientos de arena a lo largo de la costa portuguesa. La arena invadió muchos campos agrícolas y asentamientos, forzando a sus habitantes a trasladarse a otros lugares. Este artículo explora las relaciones temporales entre la ocurrencia de movimientos de arena por causa del viento y el clima, como principal impulsor de la migración de las dunas costeras. Se utilizaron fuentes históricas sobre eventos de deriva de arena como sustitutos documentales para inferir la variabilidad climática pasada en la Costa portuguesa. Se consideraron tres escalas espaciales de variabilidad climática: i) la variabilidad climática global inducida por eventos fríos abruptos durante el último milenio (LIA); ii) variabilidad climática regional (mesoescala - índice NAO); y, iii) variabilidad climática local (fenómenos meteorológicos extremos). La interpretación paleoclimática indica que los movimientos de arena en Portugal están relacionados con ambos modos del índice NAO, proporcionando nuevos conocimientos sobre la dinámica de las dunas costeras, en respuesta a las condiciones naturales. Sin embargo, la evaluación de la actividad humana en la costa también permitió comprender mejor la relación de las poblaciones locales con sus entornos, destacando que las acciones antropogénicas provocaron una alteración adicional en la dinámica de las dunas costeras.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Sand-drift events]]></kwd>
<kwd lng="en"><![CDATA[climate fluctuation]]></kwd>
<kwd lng="en"><![CDATA[LIA]]></kwd>
<kwd lng="en"><![CDATA[NAO index variability]]></kwd>
<kwd lng="en"><![CDATA[Portugal]]></kwd>
<kwd lng="pt"><![CDATA[Eventos de deriva de areia]]></kwd>
<kwd lng="pt"><![CDATA[flutuação climática]]></kwd>
<kwd lng="pt"><![CDATA[LIA]]></kwd>
<kwd lng="pt"><![CDATA[variabilidade do índice NAO]]></kwd>
<kwd lng="pt"><![CDATA[Portugal]]></kwd>
<kwd lng="fr"><![CDATA[Événements de dérive de sable]]></kwd>
<kwd lng="fr"><![CDATA[fluctuation du climat]]></kwd>
<kwd lng="fr"><![CDATA[LIA]]></kwd>
<kwd lng="fr"><![CDATA[variabilité de l&#8217;indice NAO]]></kwd>
<kwd lng="fr"><![CDATA[Portugal]]></kwd>
<kwd lng="es"><![CDATA[Eventos de deriva de arena]]></kwd>
<kwd lng="es"><![CDATA[fluctuación climática]]></kwd>
<kwd lng="es"><![CDATA[LIA]]></kwd>
<kwd lng="es"><![CDATA[variabilidad del índice NAO]]></kwd>
<kwd lng="es"><![CDATA[Portugal]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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