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description Publicationkeyboard_double_arrow_right Thesis , Doctoral thesis 2009 NetherlandsPublisher:University Library/University of Twente Authors: Sterlini van der Meer; Fenna Margreet;Sterlini van der Meer; Fenna Margreet;The sea floor of shallow seas is rarely flat and often dynamic. A widely occurring bedform type is the sand wave. Sand waves form more or less regular wavelike patterns on the seabed with crests up to one third of the water depth, wave lengths of hundreds of metres and a migration rate of metres up to tens of metres per year. Because of their migration speed and spatial dimensions, sand waves can interfere with anthropogenic activities. In relation to offshore activities especially the variation and extremes in sand wave characteristics are important. These variations can be caused by variation in environmental factors. In this thesis, we validate a non-linear idealized process-based model (Sand Wave Code, SWC) and include relevant physical processes, to relate them to variations and extremes in sand waves characteristics. Our specific interest is firstly to understand which environmental factors cause the sand wave shape and variation and, secondly, to predict this variation. First, a detailed comparison between the Golden Gate sand wave field and the SWC is carried out. The results of the SWC compare reasonably well with the observed sand waves when both an oscillating and a residual current are taken into account. Current velocity together with water depth, seem to be the most important factors influencing sand wave characteristics. Including physical processes shows that suspended sediment in general (1) shortens and lowers the sand waves, (2) increases the growth and migration rate, and (3) decreases the crest/trough ratio for the sand wave length and height. Smaller grain sizes, stronger currents, or more asymmetric currents, increase the quantitative suspended sediment effects. Surface waves, in general, lower the sand wave height and cause migration in the direction of the surface wave propagation. The shape of the sand wave changes to a broader crest, milder slopes and a smaller trough. Simulations with heterogeneous sediment indicate a coarsening trend towards the crest as observed in the North Sea. The heterogeneous sediment has no significant effect on the sand wave height and length.
NARCIS arrow_drop_down University of Twente Research Information ; NARCISDoctoral thesis . Thesis . 2009 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert NARCIS arrow_drop_down University of Twente Research Information ; NARCISDoctoral thesis . Thesis . 2009 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Netherlands, SpainPublisher:American Geophysical Union (AGU) Funded by:NWO | From small whirls to the ...NWO| From small whirls to the global ocean: how ocean eddies govern the response of the Atlantic Meridional Overturning Circulation to high-latitude climate changeSotiria Georgiou; Stefanie L. Ypma; Nils Brüggemann; Juan Manuel Sayol; Carine G. van der Boog; Paul Spence; Julie D. Pietrzak; Caroline A. Katsman;handle: 10045/112191 , 1874/421497
The dense waters formed by wintertime convection in the Labrador Sea play a key role in setting the properties of the deep Atlantic Ocean. To understand how variability in their production might affect the Atlantic Meridional Overturning Circulation (AMOC) variability, it is essential to determine pathways and associated timescales of their export. In this study, we analyze the trajectories of Argo floats and of Lagrangian particles launched at 53°N in the boundary current and traced backward in time in a high‐resolution model, to identify and quantify the importance of upstream pathways. We find that 85% of the transport carried by the particles at 53°N originates from Cape Farewell, and it is split between a direct route that follows the boundary current and an indirect route involving boundary‐interior exchanges. Although both routes contribute roughly equally to the maximum overturning, the indirect route governs its signal in denser layers. This indirect route has two branches: part of the convected water is exported rapidly on the Labrador side of the basin and part follows a longer route toward Greenland and is then carried with the boundary current. Export timescales of these two branches typically differ by 2.5 years. This study thus shows that boundary‐interior exchanges are important for the pathways and the properties of water masses arriving at 53°N. It reveals a complex three‐dimensional view of the convected water export, with implications for the arrival time of signals of variability therein at 53°N and thus for our understanding of the AMOC. S. Georgiou, S. L. Ypma, and J. ‐M. Sayol were supported by the Netherlands Organisation for Scientific Research (NWO) via VIDI grant 864.13.011 awarded to C. A. Katsman. N. Brüggemann was funded by the Collaborative Research Centre, TRR 181 “Energy Transfer in Atmosphere and Ocean” funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation, Germany) – Projektnummer 274762653. P. Spence is supported by ARC Future Fellowship FT190100413.
Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2021Full-Text: https://doi.org/10.1029/2020JC016654Data sources: Recolector de Ciencia Abierta, RECOLECTANARCIS; TU Delft RepositoryArticle . 2021Repositorio Institucional de la Universidad de AlicanteArticle . 2021Data sources: Repositorio Institucional de la Universidad de Alicanteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!visibility 13visibility views 13 download downloads 16 Powered bymore_vert Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2021Full-Text: https://doi.org/10.1029/2020JC016654Data sources: Recolector de Ciencia Abierta, RECOLECTANARCIS; TU Delft RepositoryArticle . 2021Repositorio Institucional de la Universidad de AlicanteArticle . 2021Data sources: Repositorio Institucional de la Universidad de Alicanteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021 FrancePublisher:OpenEdition Authors: Champeil-Desplats, Véronique;Champeil-Desplats, Véronique;doi: 10.4000/revdh.12079
Dans quelle mesure et comment les acteurs associatifs se donnant pour objet la défense de droits et libertés se sont saisis de la QPC et avec quel succès ? La question suppose, au préalable, de disposer de critères permettant d’identifier les acteurs associatifs concernés. Or faut-il s’attarder sur tous ceux dont une QPC a été traitée par le Conseil constitutionnel, tous agissant in fine sur le fondement de droits et libertés que la constitution garantit, ou faut-il opérer des distinctions, notamment entre des acteurs agissant pour des intérêts et ceux agissant pour des causes ? Dans ce cas, au moyen de quels critères ? Selon les réponses apportées à ces interrogations, les réalités saisies et le nombre de décisions à retenir pour analyser la part des actions associatives en faveur des droits et libertés que la constitution garantit parmi les QPC varient. Ceci peut expliquer les quelques décalages statistiques existant entre les différentes enquêtes qui ont pu être réalisées à partir de ces questionnements, même si les écarts restent globalement contenus. How associations whose purpose is to defend human rights taken up the QPC? This question presupposes pertinent criteria to identify the associations concerned. Should we focus on all those whose QPCs have been reviewed by the Constitutional Council or should we make distinctions, in particular between actors acting for interests and those acting for causes? If so, on the ground of what criteria? Depending on the answers, the corpus to and the number of decisions taken into account is variable. This may explain some statistical discrepancies between different studies on this subject.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.4000/revdh.12079&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2018 FrancePublisher:Public Library of Science (PLoS) Di Cristofaro, Julie; Mazières, Stéphane; Tous, Audrey; Di Gaetano, Cornelia; Lin, Alice A.; Nebbia, Paul; Piazza, Alberto; King, Roy J.; Underhill, Peter; Chiaroni, Jacques;International audience; The rarity of human remains makes it difficult to apprehend the first settlements in Corsica. It is admitted that initial colonization could have occurred during the Mesolithic period when glaciations would have shortened the open water travel distance from the continent. Meso-lithic sites in Corsica show relatively short and irregular occupation, and suggest discontinu-ous settling of very mobile groups probably traveling by boat. Previous genetic studies on Corsican populations showed internal differentiation and a relatively poor genetic relationship with continental populations, despite intense historical contacts, however local Meso-lithic-based genetic inheritance has never been properly estimated. The aim of this study was to explore the Corsican genetic profile of Y-chromosomes in order to trace the genetic signatures back to the first migrations to Corsica. This study included 321 samples from men throughout Corsica; samples from Provence and Tuscany were added to the cohort. All samples were typed for 92 Y-SNPs, and Y-STRs were also analyzed. Results revealed highly differentiated haplogroup patterns among Corsican populations. Haplogroup G had the highest frequency in Corsica, mostly displaying a unique Y-STR profile. When compared with Provence and Tuscany, Corsican populations displayed limited genetic proximity. Cor-sican populations present a remarkable Y-chromosome genetic mixture. Although the Cor-sican Y-chromosome profile shows similarities with both Provence and to a lesser extent Tuscany, it mainly displays its own specificity. This study confirms the high level of genetic diversity in Corsican populations and backs genetic contributions from prehistoric migrations associated with the Mesolithic, Neolithic and Metal Age eras, rather than from historical movements to Corsica, respectively attested by frequencies and TMRCA of haplogroups G2a-L91 and G2a-P15, J2a-M241 and J2-DYS445 = 6, R1b-U152 and R1b-U106. These results suggest that marine routes to reach the Corsican coast in many different points may have led to such a genetic heterogeneity.
Europe PubMed Centra... arrow_drop_down Europe PubMed CentralArticle . 2018Full-Text: http://europepmc.org/articles/PMC6070208Data sources: PubMed CentralHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2018License: CC BYFull-Text: https://hal.science/hal-01863090/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2018License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 5 citations 5 popularity Average influence Average impulse Average Powered by BIP!more_vert Europe PubMed Centra... arrow_drop_down Europe PubMed CentralArticle . 2018Full-Text: http://europepmc.org/articles/PMC6070208Data sources: PubMed CentralHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2018License: CC BYFull-Text: https://hal.science/hal-01863090/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2018License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1371/journal.pone.0200641&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Netherlands, Belgium, FrancePublisher:Elsevier BV Leon T. Hauser; Jean-Baptiste Féret; Nguyen An Binh; Niels van der Windt; Ângelo Filipe dos Reis Pereira e Cortinhas Sil; J. Timmermans; Nadejda A. Soudzilovskaia; Peter M. van Bodegom;Large-scale high-resolution satellite observations of plant functional diversity patterns will greatly benefit our ability to study ecosystem functioning. Here, we demonstrate a potentially scalable approach that uses aggregate plant traits estimated from radiative transfer model (RTM) inversion of Sentinel-2 satellite images to calculate community patterns of plant functional diversity. Trait retrieval relied on simulations and Look-up Tables (LUTs) generated by a RTM rather than heavily depending on a priori field data and data-driven statistical learning. This independence from in-situ training data benefits its scalability as relevant field data remains scarce and difficult to acquire. We ran a total of three different inversion algorithms that are representative of commonly applied approaches and we used two different metrics to calculate functional diversity. In tandem with Sentinel-2 image-based estimation of plant traits, we measured Leaf Area Index (LAI), leaf Chlorophyll content (CAB), and Leaf Mass per Area (LMA) in-situ in a (semi-)natural heterogeneous landscape (Montesinho region) located in northern Portugal. Sampling plots were scaled and georeferenced to match the satellite observed pixels and thereby allowed for a direct one-to-one posterior ground truth validation of individual traits and functional diversity. Across approaches, we observe a reasonable correspondence between the satellite-based retrievals and the insitu observations in terms of the relative distribution of individual trait means and plant functional diversity across locations despite the heterogeneity of the landscape and canopies. The functional diversity estimates, based on a combination of canopy and leaf traits, were robust against estimation biases in trait means. Particularly, the convex hull volume estimate of functional diversity showed strong concordance with in-situ observations across all three inversion methods (Spearman's rho: 0.67-0.80). The remotely sensed estimates of functional diversity also related to in-situ taxonomic diversity (Spearman's rho: 0.55-0.63). Our work highlights the potential and challenges of RTM-based functional diversity metrics to study spatial community-level ecological patterns using currently operational and publicly available Sentinel-2 imagery. While further validation and assessment across different ecosystems and larger datasets are needed, the study contributes towards a further maturation of scalable, spatially, and temporally explicit methods for functional diversity assessments from space. The authors would like to acknowledge Christian Rossi, Prof. Geof-frey M. Henebry, and the anonymous reviewers for their valuable comments and suggestions that greatly improved the manuscript. This work was supported financially by the Ecology Fund of the RoyalNetherlands Academy of Arts and Sciences (‘KNAW Fonds Ecologie’; KNAWWF/807/19011). We thank Altino Geraldes, Joao Carlos Aze-vedo, and the local farmers and foresters in the Montesinho-Nogueira Natura 2000 site for their help and collaboration. We thank Emilie Didaskalou for her lab assistance. J.-B. F ́eret acknowledges financial support from Agence Nationale de la Recherche (BioCop project—ANR- 17-32CE-0001).
NARCIS arrow_drop_down Leiden University Scholarly Publications RepositoryOther literature type . 2021License: CC BYData sources: Leiden University Scholarly Publications RepositoryMémoires en Sciences de l'Information et de la Communication; Hal-DiderotArticle . 2021License: CC BYFull-Text: https://hal.inrae.fr/hal-03245246/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 23 citations 23 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert NARCIS arrow_drop_down Leiden University Scholarly Publications RepositoryOther literature type . 2021License: CC BYData sources: Leiden University Scholarly Publications RepositoryMémoires en Sciences de l'Information et de la Communication; Hal-DiderotArticle . 2021License: CC BYFull-Text: https://hal.inrae.fr/hal-03245246/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2011 FrancePublisher:OpenEdition Authors: Antoine, Pierre; Auguste, Patrick; Bahain, Jean-Jacques; Louguet, Sophie;Antoine, Pierre; Auguste, Patrick; Bahain, Jean-Jacques; Louguet, Sophie;La paléofalaise, la formation continentale périglaciaire et le très riche gisement paléolithique moyen d’Ault-Onival (Somme) ont suscité l’intérêt des géologues et des préhistoriens depuis le début du xxe siècle. Cependant, ce site est très difficile d’accès en raison de sa localisation dans un niveau découvert seulement lors des plus basses mers, ce qui en complique l’étude. Si l’industrie lithique a fait l’objet de travaux détaillés à partir des riches assemblages provenant des prospections sur l’estran et de comparaisons avec les sites de référence de la Somme, la formation de versant périglaciaire (Formation d’Ault) n’avait jusqu’à récemment jamais été étudiée en détail. Des investigations ont donc été menées pendant plusieurs années à l’occasion des grandes marées et à la suite de périodes d’érosion de la surface des dépôts quaternaires par la mer. Des observations ont ainsi pu être effectuées sur la stratigraphie de la partie supérieure des sédiments et complétées par des sondages à la tarière et une prospection du niveau paléolithique en place. L’approche paléontologique a été basée sur l’analyse des collections conservées au Musée d’Abbeville et chez un chercheur amateur qui prospecte le site depuis de nombreuses années, mettant en exergue la présence du mammouth laineux. Les premiers résultats de cette étude permettent de confirmer un âge weichselien pour la mise en place de ces dépôts périglaciaires, ainsi que la formation du niveau durant une période pléniglaciaire. Une datation ESR/U-Th sur émail dentaire (dent de cheval) permet d’attribuer à ce niveau un âge de 55 ± 10 ka. La synthèse des données géologiques, paléontologiques et géochronologiques situe le niveau au Pléniglaciaire inférieur (SIM 4) ou à la charnière Pléniglaciaire inférieur-Pléniglaciaire moyen (SIM 4-3). Par ailleurs, la prise en compte de l’ensemble des données et du contexte structural suggère que la préservation de la Formation d’Ault est liée au rejeu récent (depuis le Pléistocène supérieur) d’une faille de direction N60-70, longeant la paléofalaise et à l’affaissement relatif du compartiment nord du substrat crayeux local. The fossil cliff, the chalky periglacial deposits and the very rich Palaeolithic site of Ault-Onival (Somme) have attracted the interest of geologists and specialists of Palaeolithic studies since the beginning of the twentieth century. This site is nevertheless very difficult to access owing to its location close to the low tide level, which therefore complicates its study. The Palaeolithic industry has already been the subject of detailed studies based on rich assemblages collected during systematic surveys of the foreshore and on comparisons with the reference sites of the Somme basin, although the periglacial deposits (Ault Formation) have never been studied in detail until now. New investigations have thus been carried out over several years during low tide episodes and also thanks to the erosion of the deposits by storms. Direct stratigraphical and sedimentological observations, complemented by hand auguring have thus been made on the upper part of the formation and completed by a survey of in situ Palaeolithic artefacts. The palaeontological study was based on the analysis of the assemblages (mainly Woolly Mammoth) preserved at the Museum of Abbeville and those collected by an amateur researcher who surveyed the site over many years. The initial results allowed confirmation of the attribution of the faunal assemblage to the Weichselian and the deposition of the sediments to a periglacial environment. ESR/U-series dating on a horse tooth provided an age of 55 ± 10 ka BP for this level. The synthesis of geological and palaeontological data, together with the geochronological results, correlate the deposits and the associated Palaeolithic site with the Weichselian Pleniglacial (MIS 4) or with the transition between MIS 4 and MIS 3 at about 58-60 ka. In addition, by taking into account previously-acquired data and the structural context, it is proposed that the preservation of the Ault Formation is linked to the movement during the Late Pleistocene of a N60-70 fault bordering the palaeo-cliff (subsidence of the northern part of the chalk bedrock).
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 4 citations 4 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book , Conference object 2014 NetherlandsPublisher:EAGE Publications BV Authors: Stanca, R.; Palcu, D. V.; Paleomagnetism; NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia;Stanca, R.; Palcu, D. V.; Paleomagnetism; NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia;handle: 1874/322701
Reviewing previous studies and adding new paleomagnetic and micropaleontologic data, this paper focuses on the Middle Miocene chronology and stratigraphy in the Dacian Basin area -a critical moment in a critical location -a choking point between the water masses of the Eastern and Central Paratethys. Firstly, it gives a new time-frame for one major tectonic, biologic and basin evolution event -the intra-Sarmatian tectonic phase -that took place in the above mentioned time interval. Secondly, it proposes a revision of the timing for one of the regional sub-stage boundaries of the Middle Miocene in Paratethys (the Volhynian and the Bessarabian). And thirdly, it offers new, reliable magnetic data from four locations that will be further used in studies regarding tectonic rotations in the Carpathian orogenic system.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert http://www.earthdoc.... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object 2014 NetherlandsPublisher:Coastal Engineering Research Council Ribberink, Jan S.; van der A, D.A.; van der Zanden, Joep; O' Donoghue, T.; Hurther, D.; Caceres, I.; Thorne, P.D.; Lynett, P.J.;First results are presented of a measurement campaign done in the large-scale Barcelona CIEM wave flume from October 2013 to January 2014. The aim of the experiments was to improve our understanding of sediment transport processes in the near-shore region. In particular, we focused on the effects of (1) wave breaking and (2) wave irregularity on net sediment transport rates and sediment transport processes. High-resolution measurements were obtained using advanced instrumentation, deployed from a custom-built measuring frame that could be horizontally and vertically positioned. These instruments provide detailed insights in the vertical distributions of sediment fluxes. Preliminary results from the breaking-wave experiments show an onshore transport of sediment prior to breaking, likely to be dominated by wave-nonlinearity effects, and an offshore sediment flux shoreward of breaking, where the sediment fluxes are undertow-dominated.
NARCIS arrow_drop_down University of Twente Research Information ; Coastal Engineering ProceedingsArticle . Conference object . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.9753/icce.v34.sediment.1&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 10 citations 10 popularity Average influence Average impulse Average Powered by BIP!more_vert NARCIS arrow_drop_down University of Twente Research Information ; Coastal Engineering ProceedingsArticle . Conference object . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.9753/icce.v34.sediment.1&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2017 FrancePublisher:Seismological Society of America (SSA) Authors: Albini, Paola; Rovida, Andrea; Scotti, Oona; Lyon-Caen, Hélène;Albini, Paola; Rovida, Andrea; Scotti, Oona; Lyon-Caen, Hélène;doi: 10.1785/0120160181
Abstract The area of the western Gulf of Corinth around the city of Aigio (Achaea, northwest Peloponnese, Greece) represents an international pilot site for continuous monitoring and multidisciplinary research on earthquake processes. In the framework of the ANR‐SISCOR Corinth Rift Laboratory project (2011–2014), a thorough reappraisal of the five largest ( M w >6) eighteenth–nineteenth century earthquakes was performed, namely those of 14 May 1748, 23 August 1817, 26 December 1861, 9 September 1888, and 25 August 1889. Written observations of earthquake effects were looked into in their original version and language and were placed in the context from which they originated, to avoid the translations and digests on which previous seismological studies had relied. Earthquake records were traced for 108 different localities, and 143 macroseismic intensities in European Macroseismic Scale 1998 (EMS‐98) have been assigned. Earthquake‐related geological phenomena have been identified and carefully mapped, to be used as a further constraint of the location and magnitude of the associated earthquakes. Finally, new parameters for the studied earthquakes have been assessed with two separate and independent strategies to quantify epistemic uncertainties. In conclusion, the 1748, 1817, and 1888 earthquakes were located in the area of Aigio; the 1861 earthquake is reckoned to be the largest in the area, with an epicentral location at sea; whereas the 1889 earthquake has been relocated to the northwest in mainland Greece, well outside the Gulf of Corinth. Electronic Supplement: Additional material and intensity values in European Macroseismic Scale 1998 (EMS‐98) for the five studied earthquakes, and tests on deriving earthquake parameters.
Bulletin of the Seis... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2017Full-Text: https://hal.science/hal-01676901/documentBulletin of the Seismological Society of AmericaArticle . 2017 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 10 citations 10 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Bulletin of the Seis... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2017Full-Text: https://hal.science/hal-01676901/documentBulletin of the Seismological Society of AmericaArticle . 2017 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2017 FrancePublisher:Springer Science and Business Media LLC Authors: Arenas-Aquino, A.R.; Matsumoto-Kuwabara, Y.; Kleiche Dray, Mina;Arenas-Aquino, A.R.; Matsumoto-Kuwabara, Y.; Kleiche Dray, Mina;pmid: 28078518
ISEBE : International Symposium of Environmental Biotechnology and Engineering, Mexico, MEX, -; Mexico City Metropolitan Area (MCMA) is the most populated urban area in the country. In 2010, MCMA required 14.8% of total energy domestic demand, but greenhouse gas emissions accounted for 7.7% of domestic emissions. Mexico has massive renewable energy potential that could be harnessed through solar photovoltaic (PV) technology. The problem to explore is the relationship between local and federal public strategies in MCMA and their stance on energy transition concern, social empowerment, new technology appropriation, and the will to boost social development and urban sustainability. A public policy typology was conducted through instruments of State intervention approach, based on political agenda articulation and environmental local interactions. Social equality is encouraged by means of forthright funding and in-kind support and energy policies focus on non-renewable energy subsidies and electric transmission infrastructure investment. There is a lack of vision for using PV technology as a guiding axis for marginalized population development. It is essential to promote economic and political rearrangement in order to level and structure environmental governance. It is essential to understand people's representation about their own needs along with renewable energy.
Horizon / Pleins tex... arrow_drop_down Environmental Science and Pollution ResearchArticle . 2017 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 5 citations 5 popularity Average influence Average impulse Average Powered by BIP!more_vert Horizon / Pleins tex... arrow_drop_down Environmental Science and Pollution ResearchArticle . 2017 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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description Publicationkeyboard_double_arrow_right Thesis , Doctoral thesis 2009 NetherlandsPublisher:University Library/University of Twente Authors: Sterlini van der Meer; Fenna Margreet;Sterlini van der Meer; Fenna Margreet;The sea floor of shallow seas is rarely flat and often dynamic. A widely occurring bedform type is the sand wave. Sand waves form more or less regular wavelike patterns on the seabed with crests up to one third of the water depth, wave lengths of hundreds of metres and a migration rate of metres up to tens of metres per year. Because of their migration speed and spatial dimensions, sand waves can interfere with anthropogenic activities. In relation to offshore activities especially the variation and extremes in sand wave characteristics are important. These variations can be caused by variation in environmental factors. In this thesis, we validate a non-linear idealized process-based model (Sand Wave Code, SWC) and include relevant physical processes, to relate them to variations and extremes in sand waves characteristics. Our specific interest is firstly to understand which environmental factors cause the sand wave shape and variation and, secondly, to predict this variation. First, a detailed comparison between the Golden Gate sand wave field and the SWC is carried out. The results of the SWC compare reasonably well with the observed sand waves when both an oscillating and a residual current are taken into account. Current velocity together with water depth, seem to be the most important factors influencing sand wave characteristics. Including physical processes shows that suspended sediment in general (1) shortens and lowers the sand waves, (2) increases the growth and migration rate, and (3) decreases the crest/trough ratio for the sand wave length and height. Smaller grain sizes, stronger currents, or more asymmetric currents, increase the quantitative suspended sediment effects. Surface waves, in general, lower the sand wave height and cause migration in the direction of the surface wave propagation. The shape of the sand wave changes to a broader crest, milder slopes and a smaller trough. Simulations with heterogeneous sediment indicate a coarsening trend towards the crest as observed in the North Sea. The heterogeneous sediment has no significant effect on the sand wave height and length.
NARCIS arrow_drop_down University of Twente Research Information ; NARCISDoctoral thesis . Thesis . 2009 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3990/1.9789036528511&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert NARCIS arrow_drop_down University of Twente Research Information ; NARCISDoctoral thesis . Thesis . 2009 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3990/1.9789036528511&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Netherlands, SpainPublisher:American Geophysical Union (AGU) Funded by:NWO | From small whirls to the ...NWO| From small whirls to the global ocean: how ocean eddies govern the response of the Atlantic Meridional Overturning Circulation to high-latitude climate changeSotiria Georgiou; Stefanie L. Ypma; Nils Brüggemann; Juan Manuel Sayol; Carine G. van der Boog; Paul Spence; Julie D. Pietrzak; Caroline A. Katsman;handle: 10045/112191 , 1874/421497
The dense waters formed by wintertime convection in the Labrador Sea play a key role in setting the properties of the deep Atlantic Ocean. To understand how variability in their production might affect the Atlantic Meridional Overturning Circulation (AMOC) variability, it is essential to determine pathways and associated timescales of their export. In this study, we analyze the trajectories of Argo floats and of Lagrangian particles launched at 53°N in the boundary current and traced backward in time in a high‐resolution model, to identify and quantify the importance of upstream pathways. We find that 85% of the transport carried by the particles at 53°N originates from Cape Farewell, and it is split between a direct route that follows the boundary current and an indirect route involving boundary‐interior exchanges. Although both routes contribute roughly equally to the maximum overturning, the indirect route governs its signal in denser layers. This indirect route has two branches: part of the convected water is exported rapidly on the Labrador side of the basin and part follows a longer route toward Greenland and is then carried with the boundary current. Export timescales of these two branches typically differ by 2.5 years. This study thus shows that boundary‐interior exchanges are important for the pathways and the properties of water masses arriving at 53°N. It reveals a complex three‐dimensional view of the convected water export, with implications for the arrival time of signals of variability therein at 53°N and thus for our understanding of the AMOC. S. Georgiou, S. L. Ypma, and J. ‐M. Sayol were supported by the Netherlands Organisation for Scientific Research (NWO) via VIDI grant 864.13.011 awarded to C. A. Katsman. N. Brüggemann was funded by the Collaborative Research Centre, TRR 181 “Energy Transfer in Atmosphere and Ocean” funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation, Germany) – Projektnummer 274762653. P. Spence is supported by ARC Future Fellowship FT190100413.
Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2021Full-Text: https://doi.org/10.1029/2020JC016654Data sources: Recolector de Ciencia Abierta, RECOLECTANARCIS; TU Delft RepositoryArticle . 2021Repositorio Institucional de la Universidad de AlicanteArticle . 2021Data sources: Repositorio Institucional de la Universidad de Alicanteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/2020jc016654&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!visibility 13visibility views 13 download downloads 16 Powered bymore_vert Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2021Full-Text: https://doi.org/10.1029/2020JC016654Data sources: Recolector de Ciencia Abierta, RECOLECTANARCIS; TU Delft RepositoryArticle . 2021Repositorio Institucional de la Universidad de AlicanteArticle . 2021Data sources: Repositorio Institucional de la Universidad de Alicanteadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1029/2020jc016654&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021 FrancePublisher:OpenEdition Authors: Champeil-Desplats, Véronique;Champeil-Desplats, Véronique;doi: 10.4000/revdh.12079
Dans quelle mesure et comment les acteurs associatifs se donnant pour objet la défense de droits et libertés se sont saisis de la QPC et avec quel succès ? La question suppose, au préalable, de disposer de critères permettant d’identifier les acteurs associatifs concernés. Or faut-il s’attarder sur tous ceux dont une QPC a été traitée par le Conseil constitutionnel, tous agissant in fine sur le fondement de droits et libertés que la constitution garantit, ou faut-il opérer des distinctions, notamment entre des acteurs agissant pour des intérêts et ceux agissant pour des causes ? Dans ce cas, au moyen de quels critères ? Selon les réponses apportées à ces interrogations, les réalités saisies et le nombre de décisions à retenir pour analyser la part des actions associatives en faveur des droits et libertés que la constitution garantit parmi les QPC varient. Ceci peut expliquer les quelques décalages statistiques existant entre les différentes enquêtes qui ont pu être réalisées à partir de ces questionnements, même si les écarts restent globalement contenus. How associations whose purpose is to defend human rights taken up the QPC? This question presupposes pertinent criteria to identify the associations concerned. Should we focus on all those whose QPCs have been reviewed by the Constitutional Council or should we make distinctions, in particular between actors acting for interests and those acting for causes? If so, on the ground of what criteria? Depending on the answers, the corpus to and the number of decisions taken into account is variable. This may explain some statistical discrepancies between different studies on this subject.
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.4000/revdh.12079&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.4000/revdh.12079&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2018 FrancePublisher:Public Library of Science (PLoS) Di Cristofaro, Julie; Mazières, Stéphane; Tous, Audrey; Di Gaetano, Cornelia; Lin, Alice A.; Nebbia, Paul; Piazza, Alberto; King, Roy J.; Underhill, Peter; Chiaroni, Jacques;International audience; The rarity of human remains makes it difficult to apprehend the first settlements in Corsica. It is admitted that initial colonization could have occurred during the Mesolithic period when glaciations would have shortened the open water travel distance from the continent. Meso-lithic sites in Corsica show relatively short and irregular occupation, and suggest discontinu-ous settling of very mobile groups probably traveling by boat. Previous genetic studies on Corsican populations showed internal differentiation and a relatively poor genetic relationship with continental populations, despite intense historical contacts, however local Meso-lithic-based genetic inheritance has never been properly estimated. The aim of this study was to explore the Corsican genetic profile of Y-chromosomes in order to trace the genetic signatures back to the first migrations to Corsica. This study included 321 samples from men throughout Corsica; samples from Provence and Tuscany were added to the cohort. All samples were typed for 92 Y-SNPs, and Y-STRs were also analyzed. Results revealed highly differentiated haplogroup patterns among Corsican populations. Haplogroup G had the highest frequency in Corsica, mostly displaying a unique Y-STR profile. When compared with Provence and Tuscany, Corsican populations displayed limited genetic proximity. Cor-sican populations present a remarkable Y-chromosome genetic mixture. Although the Cor-sican Y-chromosome profile shows similarities with both Provence and to a lesser extent Tuscany, it mainly displays its own specificity. This study confirms the high level of genetic diversity in Corsican populations and backs genetic contributions from prehistoric migrations associated with the Mesolithic, Neolithic and Metal Age eras, rather than from historical movements to Corsica, respectively attested by frequencies and TMRCA of haplogroups G2a-L91 and G2a-P15, J2a-M241 and J2-DYS445 = 6, R1b-U152 and R1b-U106. These results suggest that marine routes to reach the Corsican coast in many different points may have led to such a genetic heterogeneity.
Europe PubMed Centra... arrow_drop_down Europe PubMed CentralArticle . 2018Full-Text: http://europepmc.org/articles/PMC6070208Data sources: PubMed CentralHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2018License: CC BYFull-Text: https://hal.science/hal-01863090/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2018License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 5 citations 5 popularity Average influence Average impulse Average Powered by BIP!more_vert Europe PubMed Centra... arrow_drop_down Europe PubMed CentralArticle . 2018Full-Text: http://europepmc.org/articles/PMC6070208Data sources: PubMed CentralHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2018License: CC BYFull-Text: https://hal.science/hal-01863090/documentHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2018License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1371/journal.pone.0200641&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Netherlands, Belgium, FrancePublisher:Elsevier BV Leon T. Hauser; Jean-Baptiste Féret; Nguyen An Binh; Niels van der Windt; Ângelo Filipe dos Reis Pereira e Cortinhas Sil; J. Timmermans; Nadejda A. Soudzilovskaia; Peter M. van Bodegom;Large-scale high-resolution satellite observations of plant functional diversity patterns will greatly benefit our ability to study ecosystem functioning. Here, we demonstrate a potentially scalable approach that uses aggregate plant traits estimated from radiative transfer model (RTM) inversion of Sentinel-2 satellite images to calculate community patterns of plant functional diversity. Trait retrieval relied on simulations and Look-up Tables (LUTs) generated by a RTM rather than heavily depending on a priori field data and data-driven statistical learning. This independence from in-situ training data benefits its scalability as relevant field data remains scarce and difficult to acquire. We ran a total of three different inversion algorithms that are representative of commonly applied approaches and we used two different metrics to calculate functional diversity. In tandem with Sentinel-2 image-based estimation of plant traits, we measured Leaf Area Index (LAI), leaf Chlorophyll content (CAB), and Leaf Mass per Area (LMA) in-situ in a (semi-)natural heterogeneous landscape (Montesinho region) located in northern Portugal. Sampling plots were scaled and georeferenced to match the satellite observed pixels and thereby allowed for a direct one-to-one posterior ground truth validation of individual traits and functional diversity. Across approaches, we observe a reasonable correspondence between the satellite-based retrievals and the insitu observations in terms of the relative distribution of individual trait means and plant functional diversity across locations despite the heterogeneity of the landscape and canopies. The functional diversity estimates, based on a combination of canopy and leaf traits, were robust against estimation biases in trait means. Particularly, the convex hull volume estimate of functional diversity showed strong concordance with in-situ observations across all three inversion methods (Spearman's rho: 0.67-0.80). The remotely sensed estimates of functional diversity also related to in-situ taxonomic diversity (Spearman's rho: 0.55-0.63). Our work highlights the potential and challenges of RTM-based functional diversity metrics to study spatial community-level ecological patterns using currently operational and publicly available Sentinel-2 imagery. While further validation and assessment across different ecosystems and larger datasets are needed, the study contributes towards a further maturation of scalable, spatially, and temporally explicit methods for functional diversity assessments from space. The authors would like to acknowledge Christian Rossi, Prof. Geof-frey M. Henebry, and the anonymous reviewers for their valuable comments and suggestions that greatly improved the manuscript. This work was supported financially by the Ecology Fund of the RoyalNetherlands Academy of Arts and Sciences (‘KNAW Fonds Ecologie’; KNAWWF/807/19011). We thank Altino Geraldes, Joao Carlos Aze-vedo, and the local farmers and foresters in the Montesinho-Nogueira Natura 2000 site for their help and collaboration. We thank Emilie Didaskalou for her lab assistance. J.-B. F ́eret acknowledges financial support from Agence Nationale de la Recherche (BioCop project—ANR- 17-32CE-0001).
NARCIS arrow_drop_down Leiden University Scholarly Publications RepositoryOther literature type . 2021License: CC BYData sources: Leiden University Scholarly Publications RepositoryMémoires en Sciences de l'Information et de la Communication; Hal-DiderotArticle . 2021License: CC BYFull-Text: https://hal.inrae.fr/hal-03245246/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.rse.2021.112505&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 23 citations 23 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert NARCIS arrow_drop_down Leiden University Scholarly Publications RepositoryOther literature type . 2021License: CC BYData sources: Leiden University Scholarly Publications RepositoryMémoires en Sciences de l'Information et de la Communication; Hal-DiderotArticle . 2021License: CC BYFull-Text: https://hal.inrae.fr/hal-03245246/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.rse.2021.112505&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2011 FrancePublisher:OpenEdition Authors: Antoine, Pierre; Auguste, Patrick; Bahain, Jean-Jacques; Louguet, Sophie;Antoine, Pierre; Auguste, Patrick; Bahain, Jean-Jacques; Louguet, Sophie;La paléofalaise, la formation continentale périglaciaire et le très riche gisement paléolithique moyen d’Ault-Onival (Somme) ont suscité l’intérêt des géologues et des préhistoriens depuis le début du xxe siècle. Cependant, ce site est très difficile d’accès en raison de sa localisation dans un niveau découvert seulement lors des plus basses mers, ce qui en complique l’étude. Si l’industrie lithique a fait l’objet de travaux détaillés à partir des riches assemblages provenant des prospections sur l’estran et de comparaisons avec les sites de référence de la Somme, la formation de versant périglaciaire (Formation d’Ault) n’avait jusqu’à récemment jamais été étudiée en détail. Des investigations ont donc été menées pendant plusieurs années à l’occasion des grandes marées et à la suite de périodes d’érosion de la surface des dépôts quaternaires par la mer. Des observations ont ainsi pu être effectuées sur la stratigraphie de la partie supérieure des sédiments et complétées par des sondages à la tarière et une prospection du niveau paléolithique en place. L’approche paléontologique a été basée sur l’analyse des collections conservées au Musée d’Abbeville et chez un chercheur amateur qui prospecte le site depuis de nombreuses années, mettant en exergue la présence du mammouth laineux. Les premiers résultats de cette étude permettent de confirmer un âge weichselien pour la mise en place de ces dépôts périglaciaires, ainsi que la formation du niveau durant une période pléniglaciaire. Une datation ESR/U-Th sur émail dentaire (dent de cheval) permet d’attribuer à ce niveau un âge de 55 ± 10 ka. La synthèse des données géologiques, paléontologiques et géochronologiques situe le niveau au Pléniglaciaire inférieur (SIM 4) ou à la charnière Pléniglaciaire inférieur-Pléniglaciaire moyen (SIM 4-3). Par ailleurs, la prise en compte de l’ensemble des données et du contexte structural suggère que la préservation de la Formation d’Ault est liée au rejeu récent (depuis le Pléistocène supérieur) d’une faille de direction N60-70, longeant la paléofalaise et à l’affaissement relatif du compartiment nord du substrat crayeux local. The fossil cliff, the chalky periglacial deposits and the very rich Palaeolithic site of Ault-Onival (Somme) have attracted the interest of geologists and specialists of Palaeolithic studies since the beginning of the twentieth century. This site is nevertheless very difficult to access owing to its location close to the low tide level, which therefore complicates its study. The Palaeolithic industry has already been the subject of detailed studies based on rich assemblages collected during systematic surveys of the foreshore and on comparisons with the reference sites of the Somme basin, although the periglacial deposits (Ault Formation) have never been studied in detail until now. New investigations have thus been carried out over several years during low tide episodes and also thanks to the erosion of the deposits by storms. Direct stratigraphical and sedimentological observations, complemented by hand auguring have thus been made on the upper part of the formation and completed by a survey of in situ Palaeolithic artefacts. The palaeontological study was based on the analysis of the assemblages (mainly Woolly Mammoth) preserved at the Museum of Abbeville and those collected by an amateur researcher who surveyed the site over many years. The initial results allowed confirmation of the attribution of the faunal assemblage to the Weichselian and the deposition of the sediments to a periglacial environment. ESR/U-series dating on a horse tooth provided an age of 55 ± 10 ka BP for this level. The synthesis of geological and palaeontological data, together with the geochronological results, correlate the deposits and the associated Palaeolithic site with the Weichselian Pleniglacial (MIS 4) or with the transition between MIS 4 and MIS 3 at about 58-60 ka. In addition, by taking into account previously-acquired data and the structural context, it is proposed that the preservation of the Ault Formation is linked to the movement during the Late Pleistocene of a N60-70 fault bordering the palaeo-cliff (subsidence of the northern part of the chalk bedrock).
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.4000/quaternaire.5975&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 4 citations 4 popularity Average influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.4000/quaternaire.5975&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Part of book or chapter of book , Conference object 2014 NetherlandsPublisher:EAGE Publications BV Authors: Stanca, R.; Palcu, D. V.; Paleomagnetism; NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia;Stanca, R.; Palcu, D. V.; Paleomagnetism; NWO-VICI: The evolution of the Paratethys: the lost sea of Central Eurasia;handle: 1874/322701
Reviewing previous studies and adding new paleomagnetic and micropaleontologic data, this paper focuses on the Middle Miocene chronology and stratigraphy in the Dacian Basin area -a critical moment in a critical location -a choking point between the water masses of the Eastern and Central Paratethys. Firstly, it gives a new time-frame for one major tectonic, biologic and basin evolution event -the intra-Sarmatian tectonic phase -that took place in the above mentioned time interval. Secondly, it proposes a revision of the timing for one of the regional sub-stage boundaries of the Middle Miocene in Paratethys (the Volhynian and the Bessarabian). And thirdly, it offers new, reliable magnetic data from four locations that will be further used in studies regarding tectonic rotations in the Carpathian orogenic system.
http://www.earthdoc.... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3997/2214-4609.20140974&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert http://www.earthdoc.... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3997/2214-4609.20140974&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Conference object 2014 NetherlandsPublisher:Coastal Engineering Research Council Ribberink, Jan S.; van der A, D.A.; van der Zanden, Joep; O' Donoghue, T.; Hurther, D.; Caceres, I.; Thorne, P.D.; Lynett, P.J.;First results are presented of a measurement campaign done in the large-scale Barcelona CIEM wave flume from October 2013 to January 2014. The aim of the experiments was to improve our understanding of sediment transport processes in the near-shore region. In particular, we focused on the effects of (1) wave breaking and (2) wave irregularity on net sediment transport rates and sediment transport processes. High-resolution measurements were obtained using advanced instrumentation, deployed from a custom-built measuring frame that could be horizontally and vertically positioned. These instruments provide detailed insights in the vertical distributions of sediment fluxes. Preliminary results from the breaking-wave experiments show an onshore transport of sediment prior to breaking, likely to be dominated by wave-nonlinearity effects, and an offshore sediment flux shoreward of breaking, where the sediment fluxes are undertow-dominated.
NARCIS arrow_drop_down University of Twente Research Information ; Coastal Engineering ProceedingsArticle . Conference object . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.9753/icce.v34.sediment.1&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 10 citations 10 popularity Average influence Average impulse Average Powered by BIP!more_vert NARCIS arrow_drop_down University of Twente Research Information ; Coastal Engineering ProceedingsArticle . Conference object . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.9753/icce.v34.sediment.1&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2017 FrancePublisher:Seismological Society of America (SSA) Authors: Albini, Paola; Rovida, Andrea; Scotti, Oona; Lyon-Caen, Hélène;Albini, Paola; Rovida, Andrea; Scotti, Oona; Lyon-Caen, Hélène;doi: 10.1785/0120160181
Abstract The area of the western Gulf of Corinth around the city of Aigio (Achaea, northwest Peloponnese, Greece) represents an international pilot site for continuous monitoring and multidisciplinary research on earthquake processes. In the framework of the ANR‐SISCOR Corinth Rift Laboratory project (2011–2014), a thorough reappraisal of the five largest ( M w >6) eighteenth–nineteenth century earthquakes was performed, namely those of 14 May 1748, 23 August 1817, 26 December 1861, 9 September 1888, and 25 August 1889. Written observations of earthquake effects were looked into in their original version and language and were placed in the context from which they originated, to avoid the translations and digests on which previous seismological studies had relied. Earthquake records were traced for 108 different localities, and 143 macroseismic intensities in European Macroseismic Scale 1998 (EMS‐98) have been assigned. Earthquake‐related geological phenomena have been identified and carefully mapped, to be used as a further constraint of the location and magnitude of the associated earthquakes. Finally, new parameters for the studied earthquakes have been assessed with two separate and independent strategies to quantify epistemic uncertainties. In conclusion, the 1748, 1817, and 1888 earthquakes were located in the area of Aigio; the 1861 earthquake is reckoned to be the largest in the area, with an epicentral location at sea; whereas the 1889 earthquake has been relocated to the northwest in mainland Greece, well outside the Gulf of Corinth. Electronic Supplement: Additional material and intensity values in European Macroseismic Scale 1998 (EMS‐98) for the five studied earthquakes, and tests on deriving earthquake parameters.
Bulletin of the Seis... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2017Full-Text: https://hal.science/hal-01676901/documentBulletin of the Seismological Society of AmericaArticle . 2017 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1785/0120160181&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 10 citations 10 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Bulletin of the Seis... arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2017Full-Text: https://hal.science/hal-01676901/documentBulletin of the Seismological Society of AmericaArticle . 2017 . Peer-reviewedData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1785/0120160181&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2017 FrancePublisher:Springer Science and Business Media LLC Authors: Arenas-Aquino, A.R.; Matsumoto-Kuwabara, Y.; Kleiche Dray, Mina;Arenas-Aquino, A.R.; Matsumoto-Kuwabara, Y.; Kleiche Dray, Mina;pmid: 28078518
ISEBE : International Symposium of Environmental Biotechnology and Engineering, Mexico, MEX, -; Mexico City Metropolitan Area (MCMA) is the most populated urban area in the country. In 2010, MCMA required 14.8% of total energy domestic demand, but greenhouse gas emissions accounted for 7.7% of domestic emissions. Mexico has massive renewable energy potential that could be harnessed through solar photovoltaic (PV) technology. The problem to explore is the relationship between local and federal public strategies in MCMA and their stance on energy transition concern, social empowerment, new technology appropriation, and the will to boost social development and urban sustainability. A public policy typology was conducted through instruments of State intervention approach, based on political agenda articulation and environmental local interactions. Social equality is encouraged by means of forthright funding and in-kind support and energy policies focus on non-renewable energy subsidies and electric transmission infrastructure investment. There is a lack of vision for using PV technology as a guiding axis for marginalized population development. It is essential to promote economic and political rearrangement in order to level and structure environmental governance. It is essential to understand people's representation about their own needs along with renewable energy.
Horizon / Pleins tex... arrow_drop_down Environmental Science and Pollution ResearchArticle . 2017 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11356-017-8387-9&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 5 citations 5 popularity Average influence Average impulse Average Powered by BIP!more_vert Horizon / Pleins tex... arrow_drop_down Environmental Science and Pollution ResearchArticle . 2017 . Peer-reviewedLicense: Springer TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11356-017-8387-9&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu