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Piatt, J.F., Harding, A.M.A., Shultz, M., Speckman,S.G., Van Pelt, T.I., Drew, G.S., Kettle, A.B. (2008). Seabirds as indicators of marine food supplies: Cairns revisited. Mar. Ecol. Prog. Ser., 352, 221–234.
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Legrand M. & Mayewski P. (1997). Glaciochemistry of Polar ice cores: a review. Reviews of geophysics, 35(3), 219–243.
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. (2007). On the location of dayside magnetic reconnection during an interval of duskward oriented IMF. Annales geophysicae, 25, 219–238.
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Vacchi M., Pisano E. & La Mesa G. (1999). Ecological features of Antarctic fishes. Cold Adapted organisms. Ecophysiology Enzymology Molecular Biology, , 217–238.
Abstract: In Margesin R. & F. Schinner (eds). Cold Adapted organisms. Ecophysiology Enzymology Molecular Biology. Springer Heidelberg
Programme: 281
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. (2008). Aquat Biol, 3, 217–226.
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Hansen James, Sato Makiko, Kharecha Pushker, Beerling David, Berner Robert, Masson-Delmotte Valerie, Pagani Mark, Raymo Maureen, Royer Dana L, Zachos James C,. (2008). Target Atmospheric CO2: Where Should Humanity Aim? The Open Atmospheric Science Journal, 2(1), 217–231.
Abstract: Paleoclimate data show that climate sensitivity is ~3 deg-C for doubled CO2, including only fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks, is ~6 deg-C for doubled CO2 for the range of climate states between glacial conditions and ice-free Antarctica. Decreasing CO2 was the main cause of a cooling trend that began 50 million years ago, large scale glaciation occurring when CO2 fell to 450 +/- 100 ppm, a level that will be exceeded within decades, barring prompt policy changes. If humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, paleoclimate evidence and ongoing climate change suggest that CO2 will need to be reduced from its current 385 ppm to at most 350 ppm. The largest uncertainty in the target arises from possible changes of non-CO2 forcings. An initial 350 ppm CO2 target may be achievable by phasing out coal use except where CO2 is captured and adopting agricultural and forestry practices that sequester carbon. If the present overshoot of this target CO2 is not brief, there is a possibility of seeding irreversible catastrophic effects.
Keywords: Atmospheric and Oceanic Physics,
Programme: 458
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Van Vliet Lanoe B. & Lisitsyna O. (2001). Permafrost extent at the last glacial maximum and at the holocene optimum. The climex map. permafrost Response on Economic Development, Environmental security and Natural Resources, , 215–225.
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Koubbi P., Duhamel G., Harlay Eastwood P.D., Durand I. & Park Y.H. (2003). Distribution of larval Krefftichthys anderssoni (Myctophidae, Pisces) at the Kerguelen Archipelago (Southern Indian Ocean) modelled using GIS and habitat suitability. Antarctic biology in a global context, , 215–223.
Abstract: Antarctic biology in a global context. Huiskes A.H.L. Gieskes W.W.C. Rozema J. Schorno R.M.L. van der Vies S.M. Wolf W.J. (Eds) Backhuys Publishers Leiden
Programme: 281;373
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Krinner, G.; Magand, O.; Simmonds, I.; Genthon, C.; Dufresne, J. (2007). Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries. Climate dynamics, 28(2), 215–230.
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Yano H., Engrand C. & Maurette M. (1996). Hypervelocity impact experiments using Antarctic Micrometeorites. (Vol. XXI).
Abstract: 21 Symp. on Antarctic Meteorites, NIPR
Programme: 226
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