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Danchin E., Giraldeau L.A., Valone T.J. & Wagner R.H. (2004). Public information: from nosy neighbors to cultural evolution. Science, 305, 487–491.
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Siegenthaler U., Stocker T., Monnin E., Luthi D., Schwander J., Stauffer B., Raynaud D., Barnola J.M., Fischer H., Masson-Delmotte V. & Jouzel J. (2005). Stable Carbon Cycle-Climate Relationship During the Late Pleistocene. Science, 310, 1313–1316.
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Brook E. (2005). Tiny Bubbles Tell All. Science, 310, 1285–1287.
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Spahni R., Chappellaz J., Stocker T., Loulergue L., Hausammann G., Kawamura K., Fluckiger J., Schwander J., Raynaud D., Masson-Delmotte V. & Jouzel J. (2005). Atmospheric Methane and Nitrous Oxide of the Late Pleistocene from Antarctic Ice Cores. Science, 310, 1317–1321.
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Baroni, M.; Thiemens, M.H.; Delmas, R.J.; Savarino, J. (2007). Mass-Independent Sulfur Isotopic Compositions in Stratospheric Volcanic Eruptions. Science, 315(5808), 84–87.
Abstract: The observed mass-independent sulfur isotopic composition ({Delta}33S) of volcanic sulfate from the Agung (March 1963) and Pinatubo (June 1991) eruptions recorded in the Antarctic snow provides a mechanism for documenting stratospheric events. The sign of {Delta}33S changes over time from an initial positive component to a negative value. {Delta}33S is created during photochemical oxidation of sulfur dioxide to sulfuric acid on a monthly time scale, which indicates a fast process. The reproducibility of the results reveals that {Delta}33S is a reliable tracer to chemically identify atmospheric processes involved during stratospheric volcanism.
Programme: 457;1011
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Masson-Delmotte, V. , Jouzel, J., Landais, A., Stievenard, M. , Johnsen, S.J. , White, J.W.C. , Sveinbjornsdottir, A. , Fuhrer, K.,. (2005). Deuterium excess reveals millennial and orbital scale fluctuations of Greenland moisture origin. Science, 309, 118–121.
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Oerlemans J, Dahl-Jensen D, Masson-Delmotte V. (2006). Ice sheets and sea level. Science, 313, 1043–1044.
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Danchin, E., Giraldeau, L. A., Valone, T. J. & Wagner, R. H. (2005). Defining the Concept of Public Information – Response. Science, 308, 355–356.
Abstract: A paper that responds
to four comments on Danchin et al. 2004 Science: Dall 2005; Lotem and
Winkler 2005; Bednekoff, 2005; Laland, Coolen and Kendal 2005.
Programme: 429
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Stephens B.B., K. Gurney, P. Tans, C. Sweeney, P. Wouter, L. Bruhwiler, P.Ciais, M.Ramonet, P. Bousquet, T. Nakazawa, S. Aoki, T. Machida, G. Inoue, N. Vinnichenko, J. Lloyd, A. Jordan, O. Shibistova, R. Langenfelds, P. Steele, R. Francey, and S. Denning. (2007). The vertical distribution of atmospheric CO2 defines the latitudinal partitioning of global carbon fluxes. Science, 316, 1732–1735.
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Masson-Delmotte, V.; Jouzel, J.; Landais, A.; Stievenard, M.; Johnsen, S.J.; White, J.W.C.; Werner, M.; Sveinbjornsdottir, A.; Fuhrer, K. (2005). GRIP Deuterium Excess Reveals Rapid and Orbital-Scale Changes in Greenland Moisture Origin. Science, 309(5731), 118–121.
Abstract: The Northern Hemisphere hydrological cycle is a key factor coupling ice sheets, ocean circulation, and polar amplification of climate change. Here we present a Northern Hemisphere deuterium excess profile covering one climatic cycle, constructed with the use of {delta}18O and {delta}D Greenland Ice Core Project (GRIP) records. Past changes in Greenland source and site temperatures are quantified with precipitation seasonality taken into account. The imprint of obliquity is evidenced in the site-to-source temperature gradient at orbital scale. At the millennial time scale, GRIP source temperature changes reflect southward shifts of the geographical locations of moisture sources during cold events, and these rapid shifts are associated with large-scale changes in atmospheric circulation.
Programme: 458
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