“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 322 — #345
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322
Paléoclimatologie
Detritus Layers of the North Atlantic and their Global Climate Imprint »,
Review of Geophysics, 42, RG1005.
[16] Kageyama, M. et al. (2005), « Le Dernier Maximum glaciaire et l’événement de Heinrich 1 en termes de climat et de végétation autour de
la mer d’Alboran : une comparaison préliminaire entre modèles et données », Compte Rendus Geoscience, 337, pp. 983-992.
[17] Kageyama, M. et al. (2009), « Glacial Climate Sensitivity to Different
States of the Atlantic Meridional Overturning Circulation : Results from
the IPSL Model », Climate of the Past, 5, pp. 551-570.
[18] Kissel, C. (2005), « Magnetic Signature of Rapid Climatic Variations in
Glacial North Atlantic, a Review », Comptes Rendus Geoscience, 337,
pp. 908-918, doi:10.1016/j.crte.2005.04.009.
[19] Legrande, A. et al. (2006), « Consistent Simulations of Multiple Proxy
Responses to an Abrupt Climate Change Event », Proceedings of the National Academy of Sciences of the United States of America, 103, pp. 837842, doi:10.1073/pnas.0510095103.
[20] MacAyeal, D. R. (1993), « Binge/Purge Oscillations of the Laurentide
Ice Sheet as a Cause of the North Atlantic’s Heinrich Events », Paleoceanography, 8, pp. 775-784.
[21] Paillard, D. (2004), « Modelling Rapid Events within the Climate System », Comptes Rendus Geoscience, 336, pp. 733-740,
doi:10.1016/j.crte.2003.12.019.
[22] Peltier, W.R. and R.G. Fairbanks, 2006. Global glacial ice volume and
Last Glacial Maximum duration from an extended Barbados sea level
record, Quaternary Science Reviews, 25, pp. 3322-3337.
[23] Rasmussen, T. L. et al. (1996), « Rapid Changes in Surface and Deep
Water Conditions at the Faeroe Margin during the Last 58,000 Years »,
Paleoceanography, 11, pp. 757-771, doi:10.1029/96PA02618.
[24] Renssen, H. et al. (2001), « The 8.2 Kyr BP Event Simulated by a Global
Atmosphere-Sea-Ice-Ocean Model », Geophysical Research Letters, 28,
pp. 1 567-1 570, doi:10.1029/2000GL012602.
[25] Roche, D. M. et al. (2004), « Constraints on the Duration and Freshwater
Release of Heinrich Event 4 through Isotope Modelling », Nature, 432,
pp. 379-382, doi:10.1038/nature03059.
[26] Roche, D. M. et D. Paillard (2005), « Modelling the Oxygen-18 and Rapid
Glacial Climatic Events: A Data-Model Comparison », Comptes Rendus
Geoscience, 337, pp. 928-934, doi:10.1016/j.crte.2005.03.019.
[27] Sánchez-Goñi, M. F. et al. (2002), « Synchroneity between Marine and
Terrestrial Responses to Millennial Scale Climatic Variability during the
Last Glacial Period in the Mediterranean Region », Climate Dynamics,
19, pp. 95-105, doi:10.1007/s00382-001-0212-x.
[28] Shackleton, N. J. et al. (2000), « Phase Relationships between MillennialScale Events 64 000-24 000 Years Ago », Paleoceanography, 15, pp. 565569, doi:10.1029/2000PA000513.
i
i
i
i
i
i
i
i
322
Paléoclimatologie
Detritus Layers of the North Atlantic and their Global Climate Imprint »,
Review of Geophysics, 42, RG1005.
[16] Kageyama, M. et al. (2005), « Le Dernier Maximum glaciaire et l’événement de Heinrich 1 en termes de climat et de végétation autour de
la mer d’Alboran : une comparaison préliminaire entre modèles et données », Compte Rendus Geoscience, 337, pp. 983-992.
[17] Kageyama, M. et al. (2009), « Glacial Climate Sensitivity to Different
States of the Atlantic Meridional Overturning Circulation : Results from
the IPSL Model », Climate of the Past, 5, pp. 551-570.
[18] Kissel, C. (2005), « Magnetic Signature of Rapid Climatic Variations in
Glacial North Atlantic, a Review », Comptes Rendus Geoscience, 337,
pp. 908-918, doi:10.1016/j.crte.2005.04.009.
[19] Legrande, A. et al. (2006), « Consistent Simulations of Multiple Proxy
Responses to an Abrupt Climate Change Event », Proceedings of the National Academy of Sciences of the United States of America, 103, pp. 837842, doi:10.1073/pnas.0510095103.
[20] MacAyeal, D. R. (1993), « Binge/Purge Oscillations of the Laurentide
Ice Sheet as a Cause of the North Atlantic’s Heinrich Events », Paleoceanography, 8, pp. 775-784.
[21] Paillard, D. (2004), « Modelling Rapid Events within the Climate System », Comptes Rendus Geoscience, 336, pp. 733-740,
doi:10.1016/j.crte.2003.12.019.
[22] Peltier, W.R. and R.G. Fairbanks, 2006. Global glacial ice volume and
Last Glacial Maximum duration from an extended Barbados sea level
record, Quaternary Science Reviews, 25, pp. 3322-3337.
[23] Rasmussen, T. L. et al. (1996), « Rapid Changes in Surface and Deep
Water Conditions at the Faeroe Margin during the Last 58,000 Years »,
Paleoceanography, 11, pp. 757-771, doi:10.1029/96PA02618.
[24] Renssen, H. et al. (2001), « The 8.2 Kyr BP Event Simulated by a Global
Atmosphere-Sea-Ice-Ocean Model », Geophysical Research Letters, 28,
pp. 1 567-1 570, doi:10.1029/2000GL012602.
[25] Roche, D. M. et al. (2004), « Constraints on the Duration and Freshwater
Release of Heinrich Event 4 through Isotope Modelling », Nature, 432,
pp. 379-382, doi:10.1038/nature03059.
[26] Roche, D. M. et D. Paillard (2005), « Modelling the Oxygen-18 and Rapid
Glacial Climatic Events: A Data-Model Comparison », Comptes Rendus
Geoscience, 337, pp. 928-934, doi:10.1016/j.crte.2005.03.019.
[27] Sánchez-Goñi, M. F. et al. (2002), « Synchroneity between Marine and
Terrestrial Responses to Millennial Scale Climatic Variability during the
Last Glacial Period in the Mediterranean Region », Climate Dynamics,
19, pp. 95-105, doi:10.1007/s00382-001-0212-x.
[28] Shackleton, N. J. et al. (2000), « Phase Relationships between MillennialScale Events 64 000-24 000 Years Ago », Paleoceanography, 15, pp. 565569, doi:10.1029/2000PA000513.