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Hong S., Candelone J.P. & Boutron C.F. (1997). Changes in zinc and cadmium concentrations in Greenland ice during the past 7760 years. Atmospheric environment, 31(15), 2235–2242.
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Rivolier J., Cazes G., Dentan M.C., Rosnet E. & Vinokhodova A. (1996). Group interactions and individual behaviour during the Canadian space simulation CAPSULS. (Vol. 31).
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Rosnet E., Bachelard C., Cazes G., Dentan M.C., Le Scanff C. & Rivolier J. (1996). Influence of isolation and confinement upon the group dynamics of a 32 winteres' group. Symposium : Psychological aspects of extreme situations. (Vol. 31).
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Cooke B.D., Chapuis J.L., Magnet V., Lucas A. & Kovaliski J. (2004). Potential use of myxoma virus and rabbit haemorrhagic disease virus to control feral rabbits in the Kerguelen Archipelago. Wildl. Res., 31(4), 415–420.
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Park, Y.-H.; Roquet, F.; Vivier, F. (2004). Quasi-stationary ENSO wave signals versus the Antarctic Circumpolar Wave scenario. Geophysical research letters, 31.
Abstract: Two conflicting views on the causal mechanism of the Antarctic interannual variability often appear in the literature, i.e., whether it is remotely teleconnected to tropical ENSO events or is a self-sustained eastward propagating circumpolar wave generated locally by an ocean-atmosphere coupling mechanism. Using a Fourier decomposition into stationary and propagating components of several oceanic and atmospheric variables, we show that most of the Antarctic interannual variability can be explained by a geographically phase-locked standing wave train linked to tropical ENSO episodes. This ENSO-modulated quasi-stationary variability is not zonally uniform, rather, the strongest ENSO impact is consistently concentrated in the Pacific sector of the Southern Ocean. The eastward propagating wave component is found to be not only minor (25% of variability) but also intermittent in phase, yielding little support for the so-called Antarctic Circumpolar Wave scenario.
Keywords: 4215 Oceanography: General: Climate and interannual variability; 4207 Oceanography: General: Arctic and Antarctic oceanography; 4522 Oceanography: Physical: El Nino
Programme: 335
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Marchaudon, A.; Cerisier, J.-C.; Greenwald, R.A.; Sofko, G.J. (2004). Electrodynamics of a flux transfer event: Experimental test of the Southwood model. Geophysical research letters, 31.
Keywords: 2409 Ionosphere: Current systems; 2431 Ionosphere: Ionosphere/magnetosphere interactions; 2463 Ionosphere: Plasma convection; 2784 Magnetospheric Physics: Solar wind/magnetosphere interactions
Programme: 312;911
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Goose H., Masson-Delmotte V., Renssen H., Delmotte M., Fichefet T., Morgan V., van Ommen T., Khim B.K. & Stenni B. (2004). A delayged medieval warm period in the Southern Ocean? Geophysical research letters, 31(6), 113–117.
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Ferrari, C.P.; Dommergue, A.; Boutron, C.F.; Jitaru, P.; Adams, F.C. (2004). Profiles of Mercury in the snow pack at Station Nord, Greenland shortly after polar sunrise. Geophysical research letters, 31.
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Gilbert C., Robertson G., Le Maho Y. & Ancel A. (2006). How do weather conditions affect the huddling behaviour of emperor penguins? Polar Biol., 31(2), 163–169.
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. (2004). Can finite-frequency effects be accounted for in ray theory surface wave tomography? Geophysical research letters, 31, L24614.
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