“paleoclimatique_t2” — 2013/10/24 — 11:38 — page 427 — #450
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10. Des climats du passé aux climats du futur
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[20] Loutre, M.-F. et Berger, A. (2000), « Are We Entering an Exceptionally
Long Interglacial ? », Climatic Change, 46, pp. 61-90.
[21] Madden, R. A. et Julian, P. R. (1994), « Observations of the 40-50 Day
Tropical Oscillation: a Review », Monthly Weather Review, 122, pp. 814837.
[22] Oerlemans, J., Van der Veen, C. J. (1984), Ice Sheets and Climate, Reidel,
217 p.
[23] Oerlemans, J. (2005), « Extracting a Climate Signal from 169 Glacier
Records », Science, 308(5722), pp. 675- 677.
[24] Overpeck, J.T. et al. (2006), « Paleoclimatic Evidence for Future IceSheet Instability and Rapid Sea-Level Rise », Science, 311, pp. 1 7471 750.
[25] Peltier, W.R. (2002), « Global Glacial Isostatic Adjustment: Paleogeodetic and Space-Geodetic Tests of the ICE-4G (VM2) Model », Journal of
Quaternary Science, 17, pp. 491-510.
[26] Ramanathan, V. et Coakley, J. A. Jr. (1978), « Climate Modeling
Through Radiative-Convective Models », Reviews of Geophysics and
Space Physics, 16(4), p. 465.
[27] Ramillien, G. et al. (2006), « Interannual Variations of the Mass Balance
of the Antarctica and Greenland Ice Sheets from GRACE », Global and
Planetary Change, 53, pp. 198-208.
[28] Rigor, I. G. et Wallace, J. M. (2004), « Variations in the Age of Sea
Ice and Summer Sea Ice Extent », Geophysical Research Letters, 31,
doi:10.1029 /2004GL019492.
[29] Vautard, R. et al. (2007), « Summertime European Heat and Drought
Waves Induced by Wintertime Mediterranean Rainfall Deficit », Geophysical Research Letters, 34(L0771), doi:10.1029/2006GL028001.
[30] Velicogna, I. et Wahr, J. (2006), « Measurements of Time-Variable Gravity Show Mass Loss in Antarctica », Science, 311, pp. 1 754-1 756.
[31] Velicogna, I. (2009), « Increasing Rates of Ice Mass Loss from the Greenland and Antarctic Ice Sheets Revealed by GRACE », Geophysical Research Letters, 36 (L19503), doi:10.1029/2009GLO4022.
i
i
i
i
i
i
i
i
10. Des climats du passé aux climats du futur
427
[20] Loutre, M.-F. et Berger, A. (2000), « Are We Entering an Exceptionally
Long Interglacial ? », Climatic Change, 46, pp. 61-90.
[21] Madden, R. A. et Julian, P. R. (1994), « Observations of the 40-50 Day
Tropical Oscillation: a Review », Monthly Weather Review, 122, pp. 814837.
[22] Oerlemans, J., Van der Veen, C. J. (1984), Ice Sheets and Climate, Reidel,
217 p.
[23] Oerlemans, J. (2005), « Extracting a Climate Signal from 169 Glacier
Records », Science, 308(5722), pp. 675- 677.
[24] Overpeck, J.T. et al. (2006), « Paleoclimatic Evidence for Future IceSheet Instability and Rapid Sea-Level Rise », Science, 311, pp. 1 7471 750.
[25] Peltier, W.R. (2002), « Global Glacial Isostatic Adjustment: Paleogeodetic and Space-Geodetic Tests of the ICE-4G (VM2) Model », Journal of
Quaternary Science, 17, pp. 491-510.
[26] Ramanathan, V. et Coakley, J. A. Jr. (1978), « Climate Modeling
Through Radiative-Convective Models », Reviews of Geophysics and
Space Physics, 16(4), p. 465.
[27] Ramillien, G. et al. (2006), « Interannual Variations of the Mass Balance
of the Antarctica and Greenland Ice Sheets from GRACE », Global and
Planetary Change, 53, pp. 198-208.
[28] Rigor, I. G. et Wallace, J. M. (2004), « Variations in the Age of Sea
Ice and Summer Sea Ice Extent », Geophysical Research Letters, 31,
doi:10.1029 /2004GL019492.
[29] Vautard, R. et al. (2007), « Summertime European Heat and Drought
Waves Induced by Wintertime Mediterranean Rainfall Deficit », Geophysical Research Letters, 34(L0771), doi:10.1029/2006GL028001.
[30] Velicogna, I. et Wahr, J. (2006), « Measurements of Time-Variable Gravity Show Mass Loss in Antarctica », Science, 311, pp. 1 754-1 756.
[31] Velicogna, I. (2009), « Increasing Rates of Ice Mass Loss from the Greenland and Antarctic Ice Sheets Revealed by GRACE », Geophysical Research Letters, 36 (L19503), doi:10.1029/2009GLO4022.
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