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Charles C., Rind D., Jouzel J., Koster R. & Fairbanks R. (1994). Glacial interglacial changes in moisture sources for Greenland: influences on the ice core record of climate. Science, 261, 508–511.
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Arrigo K.R., Worthen D.L., Lizotte M.P., Dixon P. & Dieckmann G. (1997). Primary production in antarctic sea ice. Science, 276, 394–397.
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. (2002). Air-snow interactions and atmospheric chemisry. Science, 297, 1506–1510.
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Fan S.M., Gloor M., Mahlman J., Pacala S., Sarmiento J., Takahashi T. & Tans P. (1998). A large terrestrial carbon sink in North America implied by atmospheric and oceanic CO2 data and models. Science, 282, 442–446.
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Weimerskirch H., Bonadonna F., Bailleul F., Mabille G., Dell'omo G. & Lipp H.P. (2002). GPS tracking of foraging albatrosses. Science, 295, 1259.
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. (2001). An Oceanic Cold Reversal during the Last Deglaciation. Science, 293, 2074–2077.
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Caillon N., Severinghaus J.P., Jouzel J., Barnola J.M., Kang J. & Lipenkov V.Y. (2003). Timing of Atmospheric CO2 and Antarctic Temperature Changes across Termination III. Science, 299, 1728–1731.
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Morgan V.I., Delmotte M., van Ommen T.V., Jouzel J., Chappellaz J.,Woon S., Masson-Delmotte V. & Raynaud D. (2002). Relative Timing of Deglacial Climate Events in Antarctica and Greenland. Science, 297, 1862–1864.
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Bonadonna F. & Nevitt G.A. (2004). Partner-specific odor recognition in an Antarctic seabird. Science, 306, 835.
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Monnin, E.; Indermuhle, A.; Dallenbach, A.; Fluckiger, J.; Stauffer, B.; Stocker, T.F.; Raynaud, D.; Barnola, J.-M. (2001). Atmospheric CO2 Concentrations over the Last Glacial Termination. Science, 291(5501), 112–114.
Abstract: A record of atmospheric carbon dioxide (CO2) concentration during the transition from the Last Glacial Maximum to the Holocene, obtained from the Dome Concordia, Antarctica, ice core, reveals that an increase of 76 parts per million by volume occurred over a period of 6000 years in four clearly distinguishable intervals. The close correlation between CO2 concentration and Antarctic temperature indicates that the Southern Ocean played an important role in causing the CO2 increase. However, the similarity of changes in CO2 concentration and variations of atmospheric methane concentration suggests that processes in the tropics and in the Northern Hemisphere, where the main sources for methane are located, also had substantial effects on atmospheric CO2 concentrations
Programme: 960
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