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, 983–992.
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, 551–570.
Kissel, C. (2005). Magnetic signature of rapid climatic variations in
Glacial North Atlantic, a review. Comptes Rendus Geoscience, 337,
908–918. https://doi.org/10.1016/j.crte.2005.04.009.
Kobashi, T., Severinghaus, J. P., Brook, E. J., Barnola, J. M., &
Grachev, A. M. (2007). Precise timing and characterization of
abrupt climate change 8200 years ago from air trapped in polar ice.
Quaternary Science Reviews, 26(9–10), 1212–1222.
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,
837–842. https://doi.org/10.1073/pnas.0510095103.
MacAyeal, D. R. (1993). Binge/purge oscillations of the Laurentide ice
sheet as a cause of the North Atlantic’s heinrich events. Paleoceanography, 8, 775–784.
Marcott, S. A., Clark, P. U., Padman, L., Klinkhammer, G. P., Springer,
S. R., Liu, Z., et al. (2011). Ice-shelf collapse from subsurface
warming as a trigger for Heinrich events. Proceedings of the
National Academy of Sciences, 108(33), 13415–13419.
Paillard, D. (2004). Modelling rapid events within the climate system.
Comptes Rendus Geoscience, 336, 733–740. https://doi.org/10.
1016/j.crte.2003.12.019.
Peltier, W. R., & Fairbanks, R. G. (2006). Global glacial ice volume
and Last Glacial Maximum duration from an extended Barbados sea
level record. Quaternary Science Reviews, 25, 3322–3337.
Peltier, W. R., & Vettoretti, G. (2014). Dansgaard-Oeschger oscillations predicted in a comprehensive model of glacial climate: A
“kicked” salt oscillator in the Atlantic. Geophysical Research
Letters, 41(20), 7306–7313.
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,
757–771.
https://doi.org/10.1029/
96PA02618.
Rasmussen, S. O., et al. (2014). A stratigraphic framework for abrupt
climatic changes during the Last Glacial period based on three
synchronized Greenland ice-core records: refining and extending the
INTIMATE event stratigraphy. Quaternary Science Reviews, 106,
14–28. https://doi.org/10.1016/j.quascirev.2014.09.007.
Renssen, H., et al. (2001). The 8.2 Kyr BP event simulated by a global
atmosphere-sea-ice-ocean model. Geophysical Research Letters, 28,
1567–1570. https://doi.org/10.1029/2000gl012602.
Ritz, C., Rommelaere, V., & Dumas, C. (2001). Modeling the evolution
of Antarctic ice sheet over the last 420,000 years: Implications for
altitude changes in the Vostok region. Journal of Geophysical
Research: Atmospheres, 106(D23), 31943–31964.
Roberts, W. H. G., et al. (2014). A new constraint on the size of
Heinrich Events from an iceberg/sediment model. Earth and
Planetary Science Letters, 386, 1–9.
Roche, D. M., & Paillard, D. (2005). Modelling the oxygen-18 and
rapid glacial climatic events: A data-model comparison. Comptes
Rendus Geoscience, 337, 928–934. https://doi.org/10.1016/j.crte.
2005.03.019.
Roche, D. M., et al. (2004). Constraints on the duration and freshwater
release of Heinrich event 4 through isotope modelling. Nature, 432,
379–382. https://doi.org/10.1038/nature03059.
Ruddiman, W. (1977). Late quaternary deposition of ice-rafted sand in
the subpolar North Atlantic (lat 40° to 65° N), GSA Bulletin, 1813–
1827.
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, 95–105. https://doi.org/10.1007/s00382-001-0212-x.
Shackleton, N. J., et al. (2000). Phase relationships between
millennial-scale events 64,000–24,000. Paleoceanography, 15(6),
565–569.
Thomas, E. R., et al. (2007). The 8.2 Ka event from greenland ice
cores. Quaternary Science Reviews, 26, 70–81. https://doi.org/10.
1016/j.quascirev.2006.07.017.
Voelker, A. H. L., et al. (2002). Global distribution of centennial-scale
records for marine isotope stage (MIS) 3: A database, Quaternary
Science Reviews, 21, 1185–1212.
von Grafenstein, U., et al. (1998). A Mid-european decadal
isotope-climate record from 15,500 to 5000 years BP, Science,
284, 1654–1657.
Wiersma, A. P., et al. (2011). Fingerprinting the 8.2 Ka event climate
response in a coupled climate model. Journal of Quaternary
Science, 26, 118–127. https://doi.org/10.1002/jqs.1439.
29 Rapid Climate Variability: Description and Mechanisms
421
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, 983–992.
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, 551–570.
Kissel, C. (2005). Magnetic signature of rapid climatic variations in
Glacial North Atlantic, a review. Comptes Rendus Geoscience, 337,
908–918. https://doi.org/10.1016/j.crte.2005.04.009.
Kobashi, T., Severinghaus, J. P., Brook, E. J., Barnola, J. M., &
Grachev, A. M. (2007). Precise timing and characterization of
abrupt climate change 8200 years ago from air trapped in polar ice.
Quaternary Science Reviews, 26(9–10), 1212–1222.
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,
837–842. https://doi.org/10.1073/pnas.0510095103.
MacAyeal, D. R. (1993). Binge/purge oscillations of the Laurentide ice
sheet as a cause of the North Atlantic’s heinrich events. Paleoceanography, 8, 775–784.
Marcott, S. A., Clark, P. U., Padman, L., Klinkhammer, G. P., Springer,
S. R., Liu, Z., et al. (2011). Ice-shelf collapse from subsurface
warming as a trigger for Heinrich events. Proceedings of the
National Academy of Sciences, 108(33), 13415–13419.
Paillard, D. (2004). Modelling rapid events within the climate system.
Comptes Rendus Geoscience, 336, 733–740. https://doi.org/10.
1016/j.crte.2003.12.019.
Peltier, W. R., & Fairbanks, R. G. (2006). Global glacial ice volume
and Last Glacial Maximum duration from an extended Barbados sea
level record. Quaternary Science Reviews, 25, 3322–3337.
Peltier, W. R., & Vettoretti, G. (2014). Dansgaard-Oeschger oscillations predicted in a comprehensive model of glacial climate: A
“kicked” salt oscillator in the Atlantic. Geophysical Research
Letters, 41(20), 7306–7313.
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,
757–771.
https://doi.org/10.1029/
96PA02618.
Rasmussen, S. O., et al. (2014). A stratigraphic framework for abrupt
climatic changes during the Last Glacial period based on three
synchronized Greenland ice-core records: refining and extending the
INTIMATE event stratigraphy. Quaternary Science Reviews, 106,
14–28. https://doi.org/10.1016/j.quascirev.2014.09.007.
Renssen, H., et al. (2001). The 8.2 Kyr BP event simulated by a global
atmosphere-sea-ice-ocean model. Geophysical Research Letters, 28,
1567–1570. https://doi.org/10.1029/2000gl012602.
Ritz, C., Rommelaere, V., & Dumas, C. (2001). Modeling the evolution
of Antarctic ice sheet over the last 420,000 years: Implications for
altitude changes in the Vostok region. Journal of Geophysical
Research: Atmospheres, 106(D23), 31943–31964.
Roberts, W. H. G., et al. (2014). A new constraint on the size of
Heinrich Events from an iceberg/sediment model. Earth and
Planetary Science Letters, 386, 1–9.
Roche, D. M., & Paillard, D. (2005). Modelling the oxygen-18 and
rapid glacial climatic events: A data-model comparison. Comptes
Rendus Geoscience, 337, 928–934. https://doi.org/10.1016/j.crte.
2005.03.019.
Roche, D. M., et al. (2004). Constraints on the duration and freshwater
release of Heinrich event 4 through isotope modelling. Nature, 432,
379–382. https://doi.org/10.1038/nature03059.
Ruddiman, W. (1977). Late quaternary deposition of ice-rafted sand in
the subpolar North Atlantic (lat 40° to 65° N), GSA Bulletin, 1813–
1827.
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, 95–105. https://doi.org/10.1007/s00382-001-0212-x.
Shackleton, N. J., et al. (2000). Phase relationships between
millennial-scale events 64,000–24,000. Paleoceanography, 15(6),
565–569.
Thomas, E. R., et al. (2007). The 8.2 Ka event from greenland ice
cores. Quaternary Science Reviews, 26, 70–81. https://doi.org/10.
1016/j.quascirev.2006.07.017.
Voelker, A. H. L., et al. (2002). Global distribution of centennial-scale
records for marine isotope stage (MIS) 3: A database, Quaternary
Science Reviews, 21, 1185–1212.
von Grafenstein, U., et al. (1998). A Mid-european decadal
isotope-climate record from 15,500 to 5000 years BP, Science,
284, 1654–1657.
Wiersma, A. P., et al. (2011). Fingerprinting the 8.2 Ka event climate
response in a coupled climate model. Journal of Quaternary
Science, 26, 118–127. https://doi.org/10.1002/jqs.1439.
29 Rapid Climate Variability: Description and Mechanisms
421