. (2014). Energetic fitness: Linking field metabolic rates with Darwinian fitness .
Abstract: HETEROCLIM International Conference, Juin 2014, Loches
Programme: 388
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. (2014). Contributing to Pan-Arctic seabird studies.
Abstract: Annual meeting of the cBird working group of CAFF/Arctic Council. Longyearbyen-Svalbard. Mars 2014
Programme: 388
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. (2014). Contributing to Pan-Arctic seabird studies : pollutants, pathogens and parasites.
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. (2014). PLoS ONE, 9(1), e85291–.
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. (2014). Frontiers in Earth Science , 2 ( ).
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O'Connor, F.M., C.E. Johnson, O. Morgenstern, N.L. Abraham, P. Braesicke, M. Dalvi, G.A. Folberth, M.G. Sanderson, P.J. Telford, A. Voulgarakis, P.J. Young, G. Zeng, W.J. Collins, and J.A. Pyle. (2014). Evaluation of the new UKCA climate-composition model – Part 2: The Troposphere. GMD, 7, 41–91.
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Locatelli R, Bousquet P, Hourdin F, Saunois M, Cozic A, Couvreux F, Grandpeix J-Y, Lefebvre M-P, Rio C, Bergamaschi P, Chambers S D, Karstens U, Kazan V, van der Laan S, Meijer H A J, Moncrieff J, Ramonet M, Scheeren H A, Schlosser C, Schmidt M, Vermeulen A, Williams A G, . (2015). Atmospheric transport and chemistry of trace gases in LMDz5B: evaluation and implications for inverse modelling
. Geosci. Model Dev., 8(2), 129–150.
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. (2014). Terrestrial and submarine evidence for the extent and timing of the Last Glacial Maximum and the onset of deglaciation on the maritime-Antarctic and sub-Antarctic islands
. Quat Sci Rev, 100, 137–158.
Keywords: Antarctic ice sheet, Sub-Antarctica, Maritime Antarctica glaciation, Deglaciation, Quaternary, Climate,
Programme: 1048
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. (2014). A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum
. Quat Sci Rev, 100, 1–9.
Abstract: A robust understanding of Antarctic Ice Sheet deglacial history since the Last Glacial Maximum is important in order to constrain ice sheet and glacial-isostatic adjustment models, and to explore the forcing mechanisms responsible for ice sheet retreat. Such understanding can be derived from a broad range of geological and glaciological datasets and recent decades have seen an upsurge in such data gathering around the continent and Sub-Antarctic islands. Here, we report a new synthesis of those datasets, based on an accompanying series of reviews of the geological data, organised by sector. We present a series of timeslice maps for 20 ka, 15 ka, 10 ka and 5 ka, including grounding line position and ice sheet thickness changes, along with a clear assessment of levels of confidence. The reconstruction shows that the Antarctic Ice sheet did not everywhere reach the continental shelf edge at its maximum, that initial retreat was asynchronous, and that the spatial pattern of deglaciation was highly variable, particularly on the inner shelf. The deglacial reconstruction is consistent with a moderate overall excess ice volume and with a relatively small Antarctic contribution to meltwater pulse 1a. We discuss key areas of uncertainty both around the continent and by time interval, and we highlight potential priorities for future work. The synthesis is intended to be a resource for the modelling and glacial geological community.
Keywords: Antarctic Ice Sheet, Glacial geology, Modelling, Quaternary,
Programme: 1048
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. (2014).
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