REVIEWS ON GCM SIMULATIONS OF WARM CLIMATE DURING THE PAST 130 kaBP
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摘要: 回顾了国内外第四纪气候温暖期:末次间冰期(130~115 kaBP)、末次间冰阶(40~30 kaBP)的古气候模拟研究,评述了气候模拟的模式及方案、模拟实验边界条件和主要模拟结果,进而讨论第四纪温暖期的气候变化动力机制,以期进一步加深对全球气候变暖机制的认识,从而为全球温室气候变化的研究提供有益的参考。Abstract: This paper reviewed paleoclimate simulations of warm periods in the Late Quaternary, including the last interglacial (130~115 kaBP) and the megainterstadial of the last glacial (40~30 kaBP), introduced the boundary conditions of simulated experiment and essential analogue results, and discussed the mechanisms of the warm climate, in order to provide an understanding of warm climate dynamics and to recognize the further changes in the global climate.
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Key words:
- paleoclimatic simulation /
- last interglacial /
- megainterstadial of last glacial /
- warm climate /
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[1] Joussaume S, Taylor K E, Braconnot P, et al. Monsoon changes for 6000 years ago:Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)[J]. Geophysical Research Letters, 1999,26(7):859-862.
[2] Emiliani C. Pleistocene temperatures[J].Journal of Geology, 1955, 63:538-578.
[3] Bowen D Q. Quaternary Geology:A Stratigraphic Framework for Multidisciplinary Work[M]. Oxford, UK:Pergamon Press Limited,1978.
[4] Shackleton N J,Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238:oxygen isotope temperatures and ice volume on a 105 and 106 year scale[J]. Quaternary Research, 1973,3:39-55.
[5] Shackleton N J, Sánchez-Goñi M F, Pailler D, et al.Marine Isotope Substage 5e and the Eemian Interglacial[J]. Global and Planetary Change, 2003,36:151-155.
[6] Suggate R P. When did the last interglacial end?[J]. Quaternary Research,1974, 4:246-252.
[7] Shi Y F.Glacier recession and lake shrinkage indicating the climatic warming and drying trend[J]. Journal of Geographical Sciences, 1991,45(1):1-11.
[8] Shi Y F, Yu G, Liu X D, et al.Reconstruction for 30~40 kaBP enhanced Indian monsoon based on geological records from the Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169:69-83.
[9] van Andel T H.Reconstructing climate and landscape of the middle part of the last glaciation in Europe-The Stage 3 Project[J]. Quaternary Research, 2002,57:2-8.
[10] Huntley B, Tzedakis P C, de Beaulieu J -L, et al. Comparison between Biome3.5 models and pollen data[J]. Quaternary Research, 2003,59:195-212.
[11] Crowley T J,Kim K -Y. Milankovitch forcing of the last interglacial sea level[J]. Science, 1994,265:1566-1568.
[12] Royer J F, Deque M,Pestiaux P. A sensitivity experiment to astronomical forcing with a spectral GCM:simulation of the annual cycle at 125000 yrBP and 115000 yrBP[C]//Milankovitch and climate. Dordrecht, Netherlands:D. Reidel, 1984:733-736.
[13] Prell W L,Kutzbach J E. Monsoon variability over the past 150000 years[J]. Journal of Geophysical Research,1987, 92:8411-8425.
[14] Kutzbach J E, Gallimore R G,Guetter P J.Sensitivity experiments on the effect of orbitally-caused insolation changes on the interglacial climate of high northern latitudes[J]. Quaternary International, 1991,10:223-229.
[15] de Noblet N, Braconnot P, Joussaume S, et al. Sensitivity of simulated Asian and African summer monsoons to orbital induced variations in insolation 126, 115 and 6 kyrBP[J]. Climate Dynamics, 1996a,12:589-603.
[16] de Noblet N, Prentice I C, Joussaume S, et al. Possible role of atmosphere-biosphere interactions in triggering the last glaciation[J]. Geophysical Research Letters, 1996b,23(22):3191-3194.
[17] Harrison S P, Kutzbach J E, Prentice I C, et al.The response of northern hemisphere extratropical climate and vegetation to orbitally induced changes in insolation during the last interglaciation[J]. Quaternary Research, 1995, 43:174-184.
[18] Montoya M,von Storch H. Climate simulation for 125 kyr BP with a coupled ocean-atmosphere General Circulation Model[J]. Journal of Climate, 2000,13(6):1057-1072.
[19] Kubatzki C, Montoya M, Rahmstorf S, et al.Comparison of the last interglacial climate simulated by a coupled global model of intermediate complexity and an AOGCM[J]. Climate Dynamics, 2000,16:799-814.
[20] Berger A L.Long-term variations of daily insolation and Quaternary climatic changes[J]. Journal of the Atmospheric Sciences, 1978,35:2362-2367.
[21] Barnola J M, Raynaud D, Korotkevich Y S, et al.Vostok ice core provides 160000-year record of atmospheric CO2[J]. Nature, 1987, 329:408-414.
[22] Calov R, Ganopolski A, Petoukhov V, et al. Transient simulation of the last glacial inception. Part Ⅱ:sensitivity and feedback analysis[J]. Climate Dynamics, 2005,24:563-576.
[23] Petoukhov V, Ganopolski A, Brovkin V, et al. CLIMBER-2:a climate system model of intermediate complexity. Part I:model description and performance for present climate[J]. Climate Dynamics, 2000,16(1):1-7
[24] Barnola J M, Raynaud D, Korotkevich Y S, et al. Vostok ice core provides 160000-year record of atmospheric CO2[J]. Nature, 1987,329:408-414.
[25] Mikolajewicz U, Groger M, Maier-Reimer E, et al. CLIMCYC:Modeling of the Last Glacial Cycle:response of climate and vegetation to insolation forcing between 132~112 kaBP[J]. PAGES Newsletter, 2004, 12(2):24-25.
[26] Barron E J,Pollard D.High-resolution climate simulations of Oxygen Isotope Stage 3 in Europe[J]. Quaternary Research, 2002,58:296-309.
[27] Coope G R.Changes in the thermal climate in Northwestern Europe during marine oxygen isotope stage 3, estimates from fossil insect assemblages[J]. Quaternary Research, 2002,57:401-408.
[28] Alfano M J, Barron E J, Pollard D, et al.Comparison of climate model results with European vegetation and permafrost during Oxygen Isotope Stage 3[J]. Quaternary Research, 2003,59:97-107.
[29] Yu G, Zheng Y Q,Ke X K. 35 kaBP climate simulations in East Asia and probing the mechanisms of climate changes[J]. Chinese Science Bulletin,2005, 50(1):58-67.
[30] Wu G X, Liu H, Zhao Y C, et al. A nine-layer atmospheric general circulation model and its performance[J]. Advances in Atmospheric Sciences, 1996,13:1-18.
[31] Simmonds I. Analysis of the "spinning" of a global circulation model[J]. Journal of Geophysical Research, 1985,90:5637-5660.
[32] Xue Y, Sellers P J, Kinter J L, et al. A simplified biosphere model for global climate studies[J]. Journal of Climate, 1991,4:345-364.
[33] Berger A L, Loutre M F.Insolation values for the climate of the last 10 million of years[J]. Quaternary Sciences Review, 1991,10(4):297-317.
[34] Peltier W R. Ice-Age Paleotopography[J]. Science, 1994,265:195-201.
[35] Clark P U, Clague J J, Curry B B, et al. Initiation and development of the Laurentide and Cordilleran ice sheets following the last interglaciation[J]. Quaternary Science Reviews, 1993,12:79-114.
[36] Stumpf A J, Broster B E, Levson V M. Multiphase flow of the Late Wisconsinan Cordilleran ice sheet in western Canada[J]. Bulletin of the Geological Society of America, 2000,112:1850-1663.
[37] Clapperton C M, Sugden D E, Kaufman D S, et al. The last glaciation in central Magellan Strait, southernmost Chile[J]. Quaternary Research, 1995,44:133-148.
[38] Lambeck K, Chappell J. Sea level change through the last glacial cycle[J]. Science, 2001,292:679-686.
[39] Winograd I J.The magnitude and proximate cause ice sheet growth since 35000 yrBP[J]. Quaternary Research, 2001,56:299-307.
[40] Yu G, Chen X D, Ni J, et al. Palaeovegetation of China:a pollen data-based synthesis for the mid-Holocene and last glacial maximum[J]. Journal of Biogeography, 2000,27:635-664.
[41] Yu G, Xue B, Wang S M. Reconstruction of Asian palaeomonsoon patterns in China over the last 40 kyrs:A synthesis[J]. Quaternary Research, 2002,41(1):23-33.
[42] Raynaud D. The ice record of greenhouse gases[J]. Science, 1993, 259:926-934.
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