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References (53)
-
W. Ruddiman, A. Mcintyre (1976)
Northeast Atlantic Paleoclimatic Changes over the Past 600,000 YearsGeological Society of America Memoirs, 145
-
T. Crowley (1990)
Are There Any Satisfactory Geologic Analogs for a Future Greenhouse WarmingJournal of Climate, 3
-
J. Chen, H. Curran, B. White, G. Wasserburg (1991)
Precise chronology of the last interglacial period: 234U-230Th data from fossil coral reefs in the BahamasGeological Society of America Bulletin, 103
-
A. Ravelo, R. Fairbanks, S. Philander (1990)
Reconstructing tropical Atlantic hydrography using planktontic foraminifera and an ocean modelPaleoceanography, 5
-
(1990)
Anthropogenic Climate ChangesGeol. Soc. Am. Bull.
-
S. Shen, G. North, kwang-yul kim (1994)
Spectral Approach to Optimal Estimation of the Global Average TemperatureJournal of Climate, 7
-
C. Gallup, R. Edwards, Robert Johnson (1994)
The Timing of High Sea Levels Over the Past 200,000 YearsScience, 263
-
J. Guiot, J. Beaulieu, R. Cheddadi, F. David, P. Ponel, M. Reille (1993)
The climate in Western Europe during the last Glacial/Interglacial cycle derived from pollen and insect remainsPalaeogeography, Palaeoclimatology, Palaeoecology, 103
-
R. Cline, J. Hays, W. Prell, W. Ruddiman, T. Moore, N. Kipp, B. Molfino, G. Denton, T. Hughes, W. Balsam, C. Brunner, J. Duplessy, A. Esmay, J. Fastook, J. Imbrie, L. Keigwin, T. Kellogg, A. Mcintyre, R. Matthews, A. Mix, J. Morley, N. Shackleton, S. Streeter, P. Thompson (1984)
The Last Interglacial OceanQuaternary Research, 21
-
S. Joussaume, P. Braconnot (1997)
Sensitivity of paleoclimate simulation results to season definitionsJournal of Geophysical Research, 102
-
T. Crowley, kwang-yul kim (1994)
Milankovitch Forcing of the Last Interglacial Sea LevelScience, 265
-
T. Crowley (1981)
Temperature and circulation changes in the eastern North Atlantic during the last 150,000 years: Evidence from the planktonic foraminiferal recordMarine Micropaleontology, 6
-
T. J. Crowley (1981)
Temperature and circulation changes in the eastern North Atlantic during the last 150,000 years: Evidence from the planktonic foraminiferal recordJ. Clim., 6
-
N. Noblet, P. Braconnot, S. Joussaume, V. Masson (1996)
Sensitivity of simulated Asian and African summer monsoons to orbitally induced variations in insolation 126, 115 and 6 kBPClimate Dynamics, 12
-
J. Guiot, J. L. Beaulieu, R. Cheddadi, F. David, P. Ponel, M. Reille (1993)
The climate in western Europe during the last glacial/interglacial cycle derived from pollen and insect remainsJ. Geophys. Res., 103
-
A. Berger (1978)
Long-term variations of daily insolation and Quaternary climatic changesJournal of the Atmospheric Sciences, 35
-
(1976)
Mapping, and Prediction (CLIMAP) Project Members, The surface of the ice‐age EarthQuat. Res., 191
-
(1984)
The last interglacial oceanMar. Micropaleontol., 21
-
A. Vernal, C. Causse, C. Hillaire‐Marcel, R. Mott, S. Occhietti (1986)
Palynostratigraphy and Th/U ages of upper Pleistocene interglacial and interstadial deposits on Cape Breton Island, eastern CanadaGeology, 14
-
T. Guilderson, R. Fairbanks, J. Rubenstone (1994)
Tropical Temperature Variations Since 20,000 Years Ago: Modulating Interhemispheric Climate ChangeScience, 263
-
J. Hansen, I. Fung, A. Lacis, D. Rind, S. Lebedeff, R. Ruedy, G. Russell, P. Stone (1988)
Global climate changes as forecast by Goddard Institute for Space Studies three‐dimensional modelJournal of Geophysical Research, 93
-
J. Storch, V. Kharin, U. Cubasch, G. Hegerl, D. Schriever, H. Storch, E. Zorita (1997)
A Description of a 1260-Year Control Integration with the Coupled ECHAM1/LSG General Circulation ModelJournal of Climate, 10
-
M. Cracken, A. Hecht, M. Budyko, Y. Izráel' (1990)
Prospects for future climate -
T. J. Crowley (1990)
Are there any satisfactory geologic analogs for a future greenhouse warming?J. Geophys. Res., 3
-
S. P. Harrison, J. E. Kutzbach, C. E. Prentice, P. J. Behling, M. T. Sykes (1995)
The response of northern hemisphere extratropical climate and vegetation to orbitally induced changes in insolation during the last interglaciationJ. Geophys. Res., 43
-
T. Ku, Margaret Kimmel, W. Easton, T. O'neil (1974)
Eustatic Sea Level 120,000 Years Ago on Oahu, HawaiiScience, 183
-
U. Cubasch, B. Santer, A. Hellbach, G. Hegerl, H. Höck, E. Maier‐Reimer, U. Mikolajewicz, A. Stössel, R. Voss (1994)
Monte Carlo climate change forecasts with a global coupled ocean-atmosphere modelClimate Dynamics, 10
-
W. Prell, J. Kutzbach (1987)
Monsoon variability over the past 150,000 yearsJournal of Geophysical Research, 92
-
J. E. Hansen, I. Fung, A. Lacis, D. Rind, S. Lebedeff, R. Ruedy, G. Russell (1988)
Global climate changes as forecast by Goddard Institute for Space Studies three‐dimensional modelQuat. Res., 93
-
H. Storch (1992)
Inconsistencies at the interface of climate impact studies and global climate researchMeteorologische Zeitschrift, 4
-
E. Maier‐Reimer, U. Mikolajewicz, K. Hasselmann (1993)
Mean Circulation of the Hamburg LSG OGCM and Its Sensitivity to the Thermohaline Surface ForcingJournal of Physical Oceanography, 23
-
J. Mangerud, J. Svendsen (1992)
The last interglacial-glacial period on spitsbergen, SvalbardQuaternary Science Reviews, 11
-
J. Bruce, Hoesung Lee, E. Haites (1996)
Climate change 1995 -
K. Mesolella, R. Matthews, W. Broecker, D. Thurber (1969)
The Astronomical Theory of Climatic Change: Barbados DataThe Journal of Geology, 77
-
R. Edwards, J. Chen, T. Ku, G. Wasserburg (1987)
Precise Timing of the Last Interglacial Period from Mass Spectrometric Determination of Thorium-230 in CoralsScience, 236
-
J. Kutzbach, G. Bonan, J. Foley, S. Harrison (1996)
Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle HoloceneNature, 384
-
Sandy Harrison, J. Kutzbach, I. Prentice, P. Behling, Martin Sykes (1995)
The Response of Northern Hemisphere Extratropical Climate and Vegetation to Orbitally Induced Changes in Insolation during the Last InterglaciationQuaternary Research, 43
-
W. Kellog (1977)
Effects of human activities on global climate -
A. Pons, J. Guiot, J. Beaulieu, M. Reille (1992)
Recent contributions to the climatology of the last glacial-interglacial cycle based on French pollen sequencesQuaternary Science Reviews, 11
-
J. Storch (1994)
Interdecadal variability in a global coupled modelTellus A, 46
-
J. Imbrie, J. D. Hays, D. G. Martinson, A. McIntyre, A. C. Mix, J. J. Morley, N. G. Pisias, N. J. Shackleton (1984)
Milankovitch and ClimateJ. Geophys. Res.
-
William Clark, Jill Jäger (1997)
Climate Change 1995: The Science of Climate ChangeEnvironment, 39
-
T. Crowley, S. Baum (1997)
Effect of vegetation on an ice-age climate model simulationJournal of Geophysical Research, 102
-
J. Kutzbach, R. Gallimore (1988)
Sensitivity of a coupled atmosphere/mixed layer ocean model to changes in orbital forcing at 9000 years B.P.Journal of Geophysical Research, 93
-
G. Woillard (1978)
Grande Pile Peat Bog: A Continuous Pollen Record for the Last 140,000 YearsQuaternary Research, 9
-
J. Barnola, D. Raynaud, Y. Korotkevich, C. Lorius (1987)
Vostok ice core provides 160,000-year record of atmospheric CO2Nature, 329
-
N. Slowey, G. Henderson, W. Curry (1996)
Direct U–Th dating of marine sediments from the two most recent interglacial periodsNature, 383
-
U. Cubasch, K. Hasselmann, H. Höck, E. Maier‐Reimer, U. Mikolajewicz, B. Santer, R. Sausen (1992)
Time-dependent greenhouse warming computations with a coupled ocean-atmosphere modelClimate Dynamics, 8
-
E. Roeckner, K. Arpe, L. Bengtsson, S. Brinkop, L. Dümenil, M. Esch, E. Kirk, F. Lunkeit, M. Ponater, B. Rockel, R. Sausen, U. Schleese, S. Schubert, M. Windelband (1992)
Simulation of the present-day climate with the ECHAM model: Impact of model physics and resolution -
S. Bakan, A. Chlond, U. Cubasch, J. Feichter, H. Graf, H. Grassl, K. Hasselmann, I. Kirchner, M. Latif, E. Roeckner, R. Sausen, U. Schlese, D. Schriever, I. Schult, U. Schumann, F. Sielmann, W. Welke (1991)
Climate response to smoke from the burning oil wells in KuwaitNature, 351
-
R. Dodge, R. Fairbanks, L. Benninger, F. Maurrasse (1983)
Pleistocene Sea Levels from Raised Coral Reefs of HaitiScience, 219
-
R. Sausen, K. Barthel, K. Hasselmann (1988)
Coupled ocean-atmosphere models with flux correctionClimate Dynamics, 2
-
A. Bloom, W. Broecker, J. Chappell, R. Matthews, K. Mesolella (1974)
Quaternary Sea Level Fluctuations on a Tectonic coast: New 230Th/234U Dates from the Huon Peninsula, New GuineaQuaternary Research, 4
- Publisher
- Wiley
- Copyright
- Copyright © 1998 Wiley Subscription Services, Inc., A Wiley Company
- ISSN
- 0883-8305
- eISSN
- 2572-4525
- DOI
- 10.1029/97PA02550
- Publisher site
- See Article on Publisher Site
Abstract
The last interglacial (Eemian, 125,000 years ago) has generally been considered the warmest time period in the last 200,000 years and thus sometimes been used as a reference for greenhouse projections. Herein we report results from a coupled ocean‐atmosphere climate model of the surface temperature response to changes in the radiative forcing at the last interglacial. Although the model generates the expected summer warming in the northern hemisphere, winter cooling of a comparable magnitude occurs over North Africa and tropical Asia. The global annual mean temperature for the Eemian run is 0.3°C cooler than the control run. Validation of simulated sea surface temperatures (SSTs) against reconstructed SSTs supports this conclusion and also the assumption that the flux correction, fitted for the present state, operates satisfactorily for modest perturbations. Our results imply that contrary to conventional expectations, Eemian global temperatures may already have been reached by the mid 20th century.
Journal
Paleoceanography and Paleoclimatology – Wiley
Published: Apr 1, 1998