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  List of Accepted Contributions - CL24 Modelling late Quaternary climate (including Milutin Milankovic Medal Lecture)

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

Brown, K.J.; Schoups, G.; Hebda, R.J.
Reconstructing the history of precipitation across a steep moisture gradient in the coastal temperate rainforest complex of western North America

Marzin, C.; Braconnot, P.
Asian monsoon variations and teleconnections during the Holocene

Sime, L.; Quere , C.; Wolff, E.; Connolley, W.; de Boer, A.; Bopp, L.
Influence of changes in boundary conditions on Southern ocean winds at the last glacial inception

Lu, J.-M.; Kim, S.-J.
The Arctic Oscillation at the mid-Holocene and the Last Glacial Maximum: A comparison between PMIP 2 models

Peltier, W. R.
The Late-Quaternary ice-age cycel: Milankovic plus! (Milutin Milankovic Medal Lecture)

Calov, R; Ganopolski, A; Claussen, M
Simulation of Termination II

Kjellström, E.; Brandefelt, J.; Strandberg, G.; Smith, B.; Wohlfarth, B.; Näslund, J.-O.
Global and regional climate model simulations of extreme climate conditions in Sweden in a 100,000 year perspective

Crucifix, M.; Rougier, J.
Could Ruddiman's hypothesis be undecidable ?

Muri, H; Allen, M; Yamazaki, H; Henderson, G; Valdes, P
Paleo-Constraints In Ensemble Climate Modeling

Weber, S.L.; Drijfhout, S.S.
The stability of the AMOC in the Last Glacial Maximum climate

Marchal, O.; Burke, A.
Testing paleoceanographic hypotheses using inverse methods: Application to Pa-231/Th-230 data for the Heinrich Event 1

Strandberg, G; Brandefelt, J; Kjellström, E
Modelling last glacial maximum climate variability with a high resolution regional climate model

Renssen, H.; Roche, D.M.; Goosse, H.; Fichefet, T.
Modelling the impact of the Laurentide Icesheet on the timing of the Holocene thermal maximum

Fischer, N.; Jungclaus, J.; Raddatz, T.; Brovkin, V.
Eemian and Holocene Climate Variability in a Coupled Atmosphere-Ocean-Biosphere Model

Bonelli, S.; Charbit, S.; Ramstein, G.; Dumas, C.
Studying the evolution of major northern hemisphere ice sheets during marine isotopic stage 11 with a fully coupled climate-ice sheet model

Rutt, I.C.; Lunt, D.J.; Payne, A.J.; Valdes, P.J.
Ice sheet-climate coupling in the GENIE earth system model: assessment and challenges

Braconnot, P.; Marzin, C; Grégoire, L; Mosquet, E; marti, O
Monsoon response to changes in Earth’s orbital parameters : comparisons between simulations of the Eemian and of the Holocene.

Otieno, F.; Essig, M.; Oglesby, R.; Bromwich, D.
Simulating Glacial Inception at 115ka: Relative Effects of Orbital Forcing and CO2

Phipps, S. J.
Simulating the evolution of ENSO over the late Holocene (withdrawn)

Arsouze, T; Dutay, J-C; Kageyama, M; Jeandel, C; Alkama, R; Marti, O; Lacan, F
Influence of the Atlantic thermohaline circulation on neodymium isotopic composition at the last glacial maximum, a modelling sensitivity test.

Smith, R.S.; Osprey, A.; Gregory, J.M.; Browne, O.J.H; Hosoe, T.
FAMOUS-C - a new earth system model

Montoya, M.; Levermann, A.
Surface wind-stress threshold for glacial Atlantic overturning

Kageyama, M; Mignot, J; Swingedouw, D; Marzin, C; Alkama, R; Marti, O
Climate and thermohaline circulation relationships in a glacial world: a modelling study with the IPSL model

Singarayer, J; Ridgwell, A; Valdes, P
Impact of ocean circulation on glacial Pacific abyssal carbon storage and deglacial release

Schneider von Deimling, T; Ganopolski, A; Held, H; Rahmstorf, S
Are paleo-proxy data helpful for constraining future climate change?

Hoffmann, G.
Interpretation of Water Isotope Signals in paleo archives covering the last 20.000 years

Laîné, A.; Kageyama, M.; Alkama, R.; Braconnot, P.
Climatic impacts of greenhouse gas concentration changes under glacial and interglacial conditions: Polar amplification, land/sea warming ratio, atmospheric circulation impacts

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