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Culture de l'Arctique, identité nationale et enjeux circumpolaires du Canada
À la fin des années 1990, la création du Nunavut est remarquée sur le plan national et international car elle signifie la reconnaissance institutionnelle d'une... -
Analysis of aerosol transported to the Arctic based on LaMP's airborne measur...
The aims of this thesis were, in a first step, to build a climatology of pollution plumes transported from source continents to the Arctic as measured during the... -
Aérosols dans l'Arctique européen : sources, transformations et propriétés op...
Direct aerosol radiative forcing is modulated by many factors, including the chemical nature of the components and their size distribution, and the variability of... -
Microphysique du manteau neigeux : évolution de la surface spécifique de la n...
Snow covers up to 50% of land masses in the northern hemisphere in winter and its potential for interaction with the atmosphere has been demonstrated by studies in... -
On the seasonal predictability of Arctic sea ice
Sea ice experiences some major changes in the early 21st century. The recent decline of the summer Arctic sea ice extent, reaching an all-time record low in September... -
Optical properties analysis of aerosols observed in the Arctic region during ...
As part of the campaign POLARCAT France, which took place north of Sweden in April 2008, several observations of aerosol plumes were analyzed. The study of aerosol... -
Art Inuit : Formes de l'Ame et Représentations de l'Etre.
Relying on extensive field work, both in remote Arctic communities and outpost camps, and inside Canadian art collections, Cecile Pelaudeix's book presents a critical... -
Contribution of satellite remote sensing acquired in the visible, near infrar...
The overall objective of our work was to improve the knowledge of the Arctic marine environment. Using satellite remote sensing operating in the visible, near infrared... -
Dynamique du mercure dans les neiges de hautes et moyennes latitudes : études...
thèse soutenue le 2 octobre 2003 au Laboratoire de Glaciologie et Géophysique de l'Environnement
