Oral Programme CL1.10
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CL1.10 Interglacial climate change - Learning from paleoclimate archives and models (co-sponsored by the IGBP project Past Global Changes (PAGES) and the FP7 project Past4Future) |
| Convener: H. Renssen | Co-Convener: H. Fischer |
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Oral Programme
/ Thu, 26 Apr, 08:30–12:00
/ Room 16
Poster Programme
/ Attendance Thu, 26 Apr, 17:30–19:00
/ Hall X/Y
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Thursday, 26 April 2012 Room 16 Chairperson: H. Renssen |
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| 08:30–08:45 |
EGU2012-12136
Investigating annually-resovled natural climate variability during MIS 11 using lacustrine records G.J. Tye, A.P. Palmer, I. Candy, P. Coxon, and M. Hardiman |
| 08:45–09:00 |
EGU2012-375
Were the MIS 11 and MIS 5e warmer and/or wetter than the Holocene? Test comparison of Interglacial intensities using stable isotope data from Northern France tufa deposits. J. Dabkowski, N. Limondin-Lozouet, P. Antoine, A. Marca-Bell, and J. Andrews |
| 09:00–09:15 |
EGU2012-10898
The last interglacial in eastern Canada and the northwest North Atlantic : further evidence for warmer climate and ocean conditions than during the Holocene A. de Vernal, B. Fréchette, C. Hillaire-Marcel, N. van Nieuwenhove, and S. Retailleau |
| 09:15–09:30 |
EGU2012-1029
Ice Core Measurements and GCM Simulation of the Spatial Distribution and Glacial-Interglacial Change of 17O-excess in Antarctica S. Schoenemann, Q Ding, E Steig, and A Schauer |
| 09:30–09:45 |
EGU2012-10699
Holocene climate variability in south-western France D. Oliveira, F. Naughton, R. Trigo, T. Rodrigues, J-M. Jouanneau, and O. Weber |
| 09:45–10:00 |
EGU2012-9080
How variable is the Holocene? T. Laepple and P. Huybers |
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COFFEE BREAK
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| 10:30–10:45 |
EGU2012-8391
Planktic δ18O records in the northern South China Sea: MIS 5.5 vs MIS 1 M. Sarnthein and H. Sadatzki |
| 10:45–11:00 |
EGU2012-5919
Deglacial subsurface injections of Atlantic water into the Nordic Seas and its effect on interglacial climate development H.A. Bauch |
| 11:00–11:15 |
EGU2012-5058
Atmospheric circulation in the early Holocene: Sensitivity of the North Atlantic winter climate to moderate changes in the ice-sheet configuration N. Merz, C.C. Raible, and T.F. Stocker |
| 11:15–11:30 |
EGU2012-6020
Modeled vs. reconstructed δ13C variability within interglacials T. Bruecher, V. Brovkin, M. Cuntz, and C. Reick |
| 11:30–11:45 |
EGU2012-8910
The Holocene climatic optimum temperature signal from the NGRIP record. A study based on the water isotope diffusion rates as estimated from discrete high-resolution δ18O data. V. Gkinis, S. B. Simonsen, T. J. Popp, D. D. Jensen, S. L. Buchardt, B. Vinther, and S. J. Johnsen |
| 11:45–12:00 |
EGU2012-3624
Late Holocene fire activity recorded in a Greenland ice core P. Zennaro, C. Barbante, N. Kehrwald, R. Zangrando, A. Gambaro, and J. Gabrieli |