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Boutron C.F. (1999). Antarctic and Greenland Snow and Ice Cores: Archives of the cliamte and Pollution of the Atmposphere of the Earth. Korean journal of polar research, 10(2), 45–52.
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Lorius C. & Jouzel J. (1996). European project for ice coring in Antarctica (Epica)..
Abstract: The Ocean and The Poles: Grand Challenges for European Cooperation, Edited by Gotthilf Hempel, Gustav Fisher Verlag, 1996
Programme: 960
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Van De Vijver B. (1999). A protistological approach of the ecology and paleo-ecology of the subantarctic and maritime antarctic region..
Abstract: THESE, Université d'Anvers, Belgique, Thèse de Doctorat
Programme: 136
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Baker, D.F.; Law, R.M.; Gurney, K.R.; Rayner, P.; Peylin, P.; Denning, A.S.; Bousquet, P.; Bruhwiler, L.; Chen, Y.-H.; Ciais, P.; Fung, I.Y.; Heimann, M.; John, J.; Maki, T.; Maksyutov, S.; Masarie, K.; Prather, M.; Pak, B.; Taguchi, S.; Zhu, Z. (2006). TransCom 3 inversion intercomparison: Impact of transport model errors on the interannual variability of regional CO2 fluxes, 1988–2003. Global biogeochemical cycles, 20.
Abstract: Monthly CO2 fluxes are estimated across 1988–2003 for 22 emission regions using data from 78 CO2 measurement sites. The same inversion (method, priors, data) is performed with 13 different atmospheric transport models, and the spread in the results is taken as a measure of transport model error. Interannual variability (IAV) in the winds is not modeled, so any IAV in the measurements is attributed to IAV in the fluxes. When both this transport error and the random estimation errors are considered, the flux IAV obtained is statistically significant at P ? 0.05 when the fluxes are grouped into land and ocean components for three broad latitude bands, but is much less so when grouped into continents and basins. The transport errors have the largest impact in the extratropical northern latitudes. A third of the 22 emission regions have significant IAV, including the Tropical East Pacific (with physically plausible uptake/release across the 1997–2000 El Niño/La Niña) and Tropical Asia (with strong release in 1997/1998 coinciding with large-scale fires there). Most of the global IAV is attributed robustly to the tropical/southern land biosphere, including both the large release during the 1997/1998 El Niño and the post-Pinatubo uptake.
Keywords: atmospheric inversions; CO 2 fluxes; interannual variability; 0368 Atmospheric Composition and Structure: Troposphere: constituent transport and chemistry; 0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0428 Biogeosciences: Carbon cycling; 0414 Biogeosciences: Biogeochemical cycles, processes, and modeling; 3260 Mathematical Geophysics: Inverse theory
Programme: 439
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Fluteau F. (2000). Climate modeling with a 'zoom' on the polar ice sheet . The 'zoom'. French IGBP-WCRP News letter, Fevrier, 70–75.
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Genevois F. (1994). la variabilité structurelle des vocalisations et son importance dans la communication et la formation du couple chez deux espèces de Pétrels (Aves, Procellariiformes)..
Abstract: Diplôme EPHE
Programme: 109
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Jouzel J. et al. (1994). The climatic record from Antarctic ice now extends back to 220 ky BP. (Vol. 122).
Abstract: NATO Series
Programme: 254
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Moser G. (1995). Stress, réactions cognitives et comportementales : une analyse de psychologie sociale. Journal de thérapie comportementale et cognitive, 5, 3.
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Sherjal I. & Fily M. (1994). Temporal variations of microwave brightness temperatures over Antarctica. Annals of glaciology, 20, 19–25.
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Weimerskirch H. & Guionnet T. (2002). Comparative activity pattern during foraging of four albatross species. Ibis (Lond. 1859), 144, 40–50.
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