Armelle Decaulne, Najat Bhiry, Fabienne Joliet, Laine Chanteloup, Thora Martina Herrmann, Bruno Persat, Daniel Germain, Orsane Rousset. (2021). TAKUJUQ: Where Art and Science meet in Nunavik.
Abstract: The TUKISIK (Tukisigasuaqatigit: Understanding together) is a scientific program, ongoing since 2014, concerning human-environment interactions, reinforcing links between scientists and several communities.
Programme: 1148
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Noémie Martin. (2016). Suivi du trait de côte et dynamique sédimentaire des cordons littoraux du Nord-Ouest de l’Islande.
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Antoine Rocaboy. (2022). Soil microbial biomass and nutrient concentrations under the effect of vegetation cover, biological invasion and habitats of the Kerguelen Islands..
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Denis Mercier, Armelle Decaulne, Emilie Portier, Etienne Cossart. (2022). La datation des glissements de terrain paraglaciaires en Islande.
Abstract: La fonte des glaciers islandais à partir de 15ka a été suivi par des ajustements paraglaciaires dont les glissements de terrain représentent une des manifestations les plus emblématiques. Un travail d’inventaire de leur répartition spatiale permet de comptabiliser plusieurs centaines de glissements, dont 158 dans la région du Skagafjörður au Nord de l’île, 186 dans les Westfjords et 290 dans les fjords de l’est. Les logiques spatiales de leur répartition permettent de montrer un contrôle lithologique à l’échelle globale avec une surreprésentation des glissements dans les basaltes d’âge tertiaire dans des régions où les contrastes topographiques sont par ailleurs majeurs à l’échelle de l’île. Au-delà de ces éléments spatiaux, la question de l’âge de leur mise en place se pose. Si l’on compare la chronologie de la déglaciation de l’Islande avec la répartition spatiale des glissements, nous observons une décroissance de l’occurrence potentielle des glissements de terrain avec le temps. La majorité des glissements se localisent le long des versants qui ont été libérés au tout début de la déglaciation. A l’échelle des glissements eux-mêmes, des études ponctuelles permettent de préciser l’âge de leur mise en place. Différentes approches sont alors mobilisées. La première prédate les glissements en utilisant l’emboîtement des formes géomorphologiques et l’âge des plages soulevées par le rebond glacio-isostatiques sur lesquelles viennent mourir les dépôts des glissements de terrain. La seconde série de mesures postdate les glissements. En effet, des dépressions au sein des glissements ont piégé des cendres volcaniques datées et des végétaux piégés dans des tourbières. Ainsi, par téphrochronologie et datation radiocarbone, il est possible d’obtenir des dates pour caler les événements gravitaires. Les modèles âge-profondeur sont également utilisés pour affiner les résultats. Ainsi, les glissements de terrain islandais, datés avec plus ou moins de précisions, donnent des âges postglaciaires compatibles avec le schéma d’une mise en place paraglaciaire dans les tous premiers temps de l’Holocène.
Keywords: Holocene Climatic Changes Landslides Paraglacial adjustment Rock slope failures
Programme: 1266
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Denis Mercier, Emilie Portier, Armelle Decaulne, Etienne Cossart. (2022). Deep-seated gravitational slope deformation and rock-slope failures deposits in Iceland: inventory, dating and role in landscape evolution.
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Sittler, B., Lang, J., Gilg, O., Aebischer, A. (2020). Snowy owls in Greenland on the brink? Insights from 32 years of long-term monitoring on Traill Island.
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Pillet, V.; Baltzer, A.; Jensen, M.; Besset, M.; Regniers, O.; Lafon, V.; Dehouck, A.; Garestier, F. (2022). Shoreline change assessment in Svalbard Archipelago.
Abstract: Arctic coastal areas can experience higher erosion rates than temperate regions due to the combined influence of seasonal permafrost melt and extreme temperatures. In addition to these ordinary dynamics, high latitude coastal areas are even more affected by climate-induced changes such as increased weather hazards, rising temperatures or changes in river discharges and sediment supply. The Svalbard region consists of an archipelago of Arctic islands and a rocky and sandy coastline chiseled by numerous fjords connected to glaciers and a complex hydrographic network. Highly sensitive and exposed to the impacts of climate change, this coastal area is a perfect witness to the environmental changes of our century. The Svalbard Archipelago has recently become a key hotspot with an increasing number of studies, mainly focusing on glacier melt, temperature change or soil destabilization. The environmental, geographical, and geomorphological conditions of Svalbard make it extremely difficult to monitor coastal change on a large-scale. However, several studies, including Lim et al. (2020), Jaskolski et al. (2018), and Sisneros-Kidd et al. (2019), have highlighted the strong pressure of climate change, population, and human activities on the Svalbard coastal area. This littoral is fully in line with our approach to apprehend the past, present, and expected consequences of climate change on the environment and populations. In close collaboration with local researcher Maria Jensen from the University of Svalbard (UNIS) and other experts in France (Agnès Baltzer and Franck Garestier), we have explored the potential of the Copernicus Programme satellite images to produce key information on the past and recent dynamics of nearly 300 km of coastline on the archipelago. This is a major challenge, given the complexity of the environment and the meteorological and climatic conditions of the region, which limit the volume of usable spatial data (cloud cover and seasonal ice on the monitored sediments). After a first phase of adapting the algorithms to our developments, we extracted the coastline over 25 years, as well as the evolution of the banks and the extent of the hydrographic network along several major fjords in Svalbard. Particular attention was given to Advenfjorden to improve our effort, due to the greater availability of data to validate our results. We experienced the bathymetric monitoring into the fjord. This information was one of the most complex challenge in terms of methodology and algorithm development regarding the environmental context, but it is also a crucial insight to consider the full climate change impact on coastal sediment dynamics. Finally, we extracted another coastal indicator to focus on changes in the deltaic areas, namely the pioneer vegetation coverage, which reveals the impact of warming on these highly dynamic regions. For the first time, we present our new results issued from these investigations.
Programme: 1223
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Michael Lockwood, Mathew J. Owens, Carl Haines, Luke Barnard, Christopher John Scott, Aude Chambodut, Kathryn A. McWilliams, Alan W. P. Thomson. (2020). Universal Time Variations in Space Weather (Vol. 12).
Abstract: We introduce the inductive effects of polar cap motions towards and way from the Sun into magnetospheric electrodynamics and show how this explains observed Universal Time variations in hemispheric geomagnetic indices. The large (and growing) hemispheric asymmetry in the offsets of the geomagnetic (dip or eccentric dipole) poles from Earth’s rotational axis means that the effect is not cancelled out in global indices. By adding this effect to that of the Russell-McPherron effect on solar wind-magnetosphere coupling, that of ionospheric conductivities, and that of the solar wind dynamic pressure and dipole tilt on the near-Earth tail lobe field and cross-tail current sheet, we are able to model the persistent “equinoctial” time-of-day/time-of-year pattern (with additional net Universal time variations) observed in the an, as and am geomagnetic indices since 1959. We discuss the implications for the longitudinal dependence of the effects of extreme space weather events
Programme: 139
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Bruyant, F., Amiraux, R., Amyot, M. P., Archambault, P., Artigue, L., Bardedo de Freitas, L., ...Fort, J.,... & Babin, M. (2022). The Green Edge cruise: Understanding the onset, life and fate of the Arctic phytoplankton spring bloom.
Abstract: The Green Edge project was designed to investigate the onset, life and fate of a phytoplankton spring bloom (PSB) in the Arctic Ocean. The lengthening of the ice-free period and the warming of seawater, amongst other factors, have induced major changes in arctic ocean biology over the last decades. Because the PSB is at the base of the Arctic Ocean food chain, it is crucial to understand how changes in the arctic environment will affect it. Green Edge was a large multidisciplinary collaborative project bringing researchers and technicians from 28 different institutions in seven countries, together aiming at understanding these changes and their impacts into the future. The fieldwork for the Green Edge project took place over two years (2015 and 2016) and was carried out from both an ice-camp and a research vessel in the Baffin Bay, canadian arctic. This paper describes the sampling strategy and the data set obtained from the research cruise, which took place aboard the Canadian Coast Guard Ship (CCGS) Amundsen in spring 2016. The dataset is available at https://doi.org/10.17882/59892 (Massicotte et al., 2019a).
Programme: 388
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Antoine Grisart, Mathieu Casado, Vasileios Gkinis, Bo Vinther, Philippe Naveau, Mathieu Vrac, Thomas Laepple, Bénédicte Minster, Fréderic Prié, Barbara Stenni, Elise Fourré, Hans-Christian Steen Larsen, Jean Jouzel, Martin Werner, Katy Pol, Valérie Masson-Delmotte, Maria Hoerhold, Trevor Popp, Amaelle Landais. (2022). Sub-millennial climate variability from high resolution water isotopes in the EDC ice core.
Abstract: The EPICA Dome C (EDC) ice core provides the longest continuous climatic record covering the last 800 000 years (800 kyrs). Obtaining homogeneous high resolution measurements and accounting for diffusion provide a unique opportunity to study the evolution of decadal to millennial variability within the past glacial and interglacial periods. We present here a compilation of high resolution (11 cm) water isotopic records with 27 000 δ18O measurements and 7 920 δD measurements (covering respectively 94 % and 27 % of the whole EDC record), including published and new measurements (2 900 for both δ18O and δD) over the last 800 kyrs on the EDC ice core. We show that overlapping measurement series performed over multiple depth ranges over the past 20 years, using different analytical methods and in different laboratories, are consistent within analytical uncertainty, and therefore can be combined to provide a homogeneous data set. A frequency decomposition of the most complete δ18O record and a simple assessment of the possible influence of diffusion on the measured profile shows that the variability during glacial periods at multi-decadal to multi-centennial timescale is higher than variability of the interglacial periods. This analysis shows as well that during interglacial periods characterized by a temperature optimum at its beginning, the multi-centennial variability is the strongest over this temperature optimum.
Programme: 1110
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