|
|
Scanff C., Larue J. & Rosnet E L.E. (1997). How to measure human adaptation in extreme environment: The case of Antarctic winter-owering. Aviation space and environmental medicine, 68(12), 1144–1149.
|
|
|
|
Chappellaz J., Raynaud D., Blunier T. & Stauffer B. (2000). The Ice core record of Atmospheric Methane..
Abstract: In Mohamed Aslam Khan Khalil (Ed.) Atmospheric Methane, Springer-Verlag Berlin Heidelberg
Programme: 159
|
|
|
|
Godin S., Guirlet M. & David C. (1995). Effect of the Mount Pinatubo Volcanic cloud on Stratospheric Ozone Amounts Monitored at OHP (44°N, 6°E) and Dumont d'Urville (66°S, 140°E)..
Abstract: IUGG, Boulder
Programme: 209
|
|
|
|
Micol T. & Jouventin P. (1998). Le retour des oiseaux sur l'île de Saint-Paul. Pour la science, 251, 21.
|
|
|
|
Bousquet, P.; Ciais, P.; Peylin, P.; Ramonet, M.; Monfray, P. (1999). Inverse modeling of annual atmospheric CO2 sources and sinks 1. Method and control inversion. J. Geophys. Res., 104(d21), 26,161–26,178.
Abstract: A primary goal of developing the CO2 atmospheric measurement network is to better characterize the sources and sinks of atmospheric CO2. Atmospheric transport models can be used to interpret atmospheric measurements in terms of surface fluxes using inverse methodology. In this paper we present a three-dimensional (3-D) inversion of CO2 measurements in order to infer annual sources and sinks of CO2 at a continental scale (continents and ocean basins) for a climatological year representing the 1985–1995 period. Solving this inverse problem requires (1) a data space representing monthly CO2 measurements, here at 77 sites (surface, ships, planes), (2) a flux space describing a priori fluxes between carbon reservoirs, and (3) a 3-D transport model linking the flux space to the data space. Knowledge of these three elements, together with their associated errors, allows one to reduce the uncertainties of the CO2 sources and sinks. In the 1985–1995 period, for our control inversion, the global continental sink is found to be 2.7±1.5 Gt C yr1 for an optimized deforestation source of 1.4±0.6 Gt C yr1, yielding a net land uptake of 1.3±1.6 Gt C yr1 (fossil fuel removed). The continental partition of this budget is (in units of Gt C yr1): Arctic +0.2±0.3, North America ?0.5±0.6, Europe ?0.3±0.8, north Asia ?1.5±0.7, tropics (except Asia) +0.3±0.9, tropical Asia +0.8±0.4, and Southern Hemisphere ?0.1±0.3. The inferred partition for the controversial Northern Hemisphere CO2 sink reveals that a major sink is located over the north Asia continent. For oceans we find a net global sink of 1.5±0.5 Gt C yr1 with the following partition (in units of Gt C yr1): North Pacific ?0.3±0.2, North Atlantic ?0.8±0.3, equator +0.6±0.2, 20°S–50°S oceans ?0.9±0.3, and austral ocean ?0.1±0.1.
Programme: 146;344
|
|
|
|
Cherel, Y. and N. Klages. (1998). A review of the food of albatrosses.
Abstract: In: G. Robertson and R. Gales (eds.)
Albatross biology and conservation. Chipping Norton: Surrey Beatty & Sons.
Programme: 109
|
|
|
|
Gerday C. (1998). The cold adaptated Ca²+-Zn²+ protease from the antarctic psychrophile Pseudomonas sp.TAC18..
Abstract: Eurocold meeting
Programme: 193
|
|
|
|
Duhamel G. (1995). Stock discrimination at the Kerguelen Plateau: Champsocephalus gunnari and Dissostichus eleginoides. Bachelor's thesis, , .
Abstract: Geneflow Workshop, British Antarctic Survey 28-29 November 1995, Abstracts and Workshop Report
Programme: 180
|
|
|
|
Kanakidou, M., P.J. Crutzen, P.H. Zimmermann and B. Bonsang. (1992). A 3-dimensional global study of the photochemistry of ethane and propane in the troposphere: Production and transport of organic nitrogen compounds.
Abstract: In: “Air Pollution Modeling and its Application IX”, H. van Dop and G. Kallos (Eds.), Plenum Press, New York, 415-426 (1992).
Programme: 146
|
|
|
|
Gagnevin D. (1998). La série volcanique alcaline néogène de la caldera de la péninsule Rallier-du-Baty (Kerguelen, TAAF): Etude pétrologique et géochimique..
Abstract: Maîtrise de Sciences de la Terre
Programme: 251
|
|
