“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 426 — #449
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[7] Cazenave, A. et al. (2009), « Sea Level Budget over 2003-2008: A Reevaluation from GRACE Space Gravimetry ; Satellite Altimetry and Argo »,
Global and Planetary Change, 65, pp. 83-88.
[8] Charbit, S. et al. (2008), « Amount of CO 2 Emissions Irreversibly Leading to the Total Melting of Greenland », Geophysical Research Letters,
35(L12503), doi:10.1029/2008GLO33472.
[9] Chen, J. L. et al. (2006), « Satellite Gravity Measurements
Confirm Accelerated Melting of Greenland Ice Sheet », Science, 313,
doi:10.1126/science.1129007.
[10] DeConto, R. M. et Pollard, D. (2003), « Rapid Cenozoic Glaciation of Antarctica Induced by Declining Atmospheric CO 2 », Nature, 421, pp. 245249, doi:10.1038/nature01290.
[11] Dufresne, J.-L. et al. (2006), « Simulation de l’évolution récente et future
du climat par les modèles du CNRM et de l’IPSL (Recent and Futur
Climate Change as Simulated by the CNRM and IPSL Models) », La
Météorologie, 55, pp. 45-59.
[12] Dufresne, J.-L. et Bony, S. (2008), « An Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled
Atmosphere-Ocean Models », Journal of Climate, 21(19), pp. 5 135-5 144,
doi: 10.1175/2008JCLI2239.1.
[13] Fettweis, X. et al. (2008), « Estimation of the Greenland Ice Sheet Surface Mass Balance for the 20
th and 21
st Centuries », The Cryopshere, 2,
pp. 117-129.
[14] Gallée, H. et al. (1992), « Simulation of the Last Glacial Cycle by a Coupled, Sectorially Averaged Climate-Ice-Sheet Model 2. Response to Insolation and CO 2 Variations », Journal of Geophysical Research, 97(D14),
pp. 15 713-15 740.
[15] IPCC (Ed.), Climate Change (2007): The Physical Science Basis ;
Contribution of Working Group I to the Fourth Assessment Report of the
Intergovernmental Panel on Climate Change, Cambridge, United Kingdom, and New-York, USA, Cambridge University Press.
[16] Keeling, C. D. et al. (1995), « Interannual Extremes in the Rate of Rise
of Atmospheric Carbon Dioxide since 1980 », Nature, 375, pp. 666-670.
[17] Khodri, M. et al. (2001), « Simulating the Amplification of Orbital Forcing by Ocean Feedbacks in the Last Glaciation », Nature, 410, pp. 570574.
[18] Krinner, G. et al. (2007), « Simulated Antarctic Precipitation and Surface Mass Balance at the End of the 20
th and 21
st Centuries », Climate
Dynamics, 28, pp. 215-230, doi:10.1007/s00382-006-0177.
[19] Lambert, S. J. et Fyfe, J. C. (2006), « Changes in Winter Cyclone Frequencies and Strengths Simulated in Enhanced Greenhouse Warming Experiments: Results from the Models Participating in the IPCC Diagnostic
Exercise », Climate Dynamics, 26, pp. 713-728, doi: 10.1007/s00382-0060110-3.
i
i
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i
i
426
Paléoclimatologie
[7] Cazenave, A. et al. (2009), « Sea Level Budget over 2003-2008: A Reevaluation from GRACE Space Gravimetry ; Satellite Altimetry and Argo »,
Global and Planetary Change, 65, pp. 83-88.
[8] Charbit, S. et al. (2008), « Amount of CO 2 Emissions Irreversibly Leading to the Total Melting of Greenland », Geophysical Research Letters,
35(L12503), doi:10.1029/2008GLO33472.
[9] Chen, J. L. et al. (2006), « Satellite Gravity Measurements
Confirm Accelerated Melting of Greenland Ice Sheet », Science, 313,
doi:10.1126/science.1129007.
[10] DeConto, R. M. et Pollard, D. (2003), « Rapid Cenozoic Glaciation of Antarctica Induced by Declining Atmospheric CO 2 », Nature, 421, pp. 245249, doi:10.1038/nature01290.
[11] Dufresne, J.-L. et al. (2006), « Simulation de l’évolution récente et future
du climat par les modèles du CNRM et de l’IPSL (Recent and Futur
Climate Change as Simulated by the CNRM and IPSL Models) », La
Météorologie, 55, pp. 45-59.
[12] Dufresne, J.-L. et Bony, S. (2008), « An Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled
Atmosphere-Ocean Models », Journal of Climate, 21(19), pp. 5 135-5 144,
doi: 10.1175/2008JCLI2239.1.
[13] Fettweis, X. et al. (2008), « Estimation of the Greenland Ice Sheet Surface Mass Balance for the 20
th and 21
st Centuries », The Cryopshere, 2,
pp. 117-129.
[14] Gallée, H. et al. (1992), « Simulation of the Last Glacial Cycle by a Coupled, Sectorially Averaged Climate-Ice-Sheet Model 2. Response to Insolation and CO 2 Variations », Journal of Geophysical Research, 97(D14),
pp. 15 713-15 740.
[15] IPCC (Ed.), Climate Change (2007): The Physical Science Basis ;
Contribution of Working Group I to the Fourth Assessment Report of the
Intergovernmental Panel on Climate Change, Cambridge, United Kingdom, and New-York, USA, Cambridge University Press.
[16] Keeling, C. D. et al. (1995), « Interannual Extremes in the Rate of Rise
of Atmospheric Carbon Dioxide since 1980 », Nature, 375, pp. 666-670.
[17] Khodri, M. et al. (2001), « Simulating the Amplification of Orbital Forcing by Ocean Feedbacks in the Last Glaciation », Nature, 410, pp. 570574.
[18] Krinner, G. et al. (2007), « Simulated Antarctic Precipitation and Surface Mass Balance at the End of the 20
th and 21
st Centuries », Climate
Dynamics, 28, pp. 215-230, doi:10.1007/s00382-006-0177.
[19] Lambert, S. J. et Fyfe, J. C. (2006), « Changes in Winter Cyclone Frequencies and Strengths Simulated in Enhanced Greenhouse Warming Experiments: Results from the Models Participating in the IPCC Diagnostic
Exercise », Climate Dynamics, 26, pp. 713-728, doi: 10.1007/s00382-0060110-3.