Joussaume S,Taylor K E.Status of the Palaeoelimate Modeling Intercomparison Project(PMIP).In:Gates W L ed.Proceedings of the First International AMIP Scientific Conference.15～19 May 1995,WCRP Report No.92.Geneva,Monterey,California,USA,1995.425～430
[2]
吴乃琴,吕厚远,孙湘君等.植物硅酸体-气候因子转换函数及其在渭南晚冰期以来古环境研究中的应用.第四纪研究,1994,(3):270～279 Wu Naiqin,Lü Houyuan,Sun Xiangjun et al.Climate transfer function from opal phytolith and its application in paleoclimate reconstruction of China loess-paleosol sequence.Quaternary Sciences,1994,(3):270～279
[3]
秦伯强,施雅风,于革.亚洲内陆湖泊在18kaBP及6kaB.P.的水位变化及其指示意义.科学通报,1997,42(24):2586～2596 Qin Boqiang,Shi Yafeng,Yu Ge,The reconstruction and interpretations of lake status at 6ka and 18 kaB.P.in inland Asia.Chinese Science Bulletin,1998,43(14):1145～1157
[4]
施雅风,郑本兴,姚檀栋.青藏高原末次冰期最盛时的冰川与环境.冰川冻土,1997,19(2):97～113 Shi Yafeng,Zheng Benxing,Yao Tandong.Glaciers and environments during the Last Glacial Maximum(LGM)on the Tibetan Plateau.Journal of Glaciology and Geocryology,1997,19(2):97～113
[5]
姚檀栋,Thompson L G,施雅风等.古里雅冰芯中末次间期以来气候变化记录研究.中国科学(D辑),1997,27(5):447～452 Yao Tandong,Thompson L G,Shi Yafeng et al.Climate variation since the Last Interglaciation recorded in the Guliya ice core.Science in China(Series D),1997,27(6):662～668
[6]
刘东生,张新时,熊尚发等.青藏高原冰期环境与冰期全球降温.第四纪研究,1999,(5):385～396 Liu Tungsheng,Zhang Xinshi,Xiong Shangfa et al.Qinghai-Xizang Plateau glacial environment and global cooling.Quaternary Sciences,1999,(5):385～396
[7]
王宁练,姚檀栋,施雅风等.末次冰盛期时赤道地区的降温幅度问题.中国科学(D辑),1999,29(增刊1):70～78 Wang Ninglian,Yao Tandong,Shi Yafeng et al.On the magnitude of temperature decrease in the equatorial regions during the Last Glacial Maximum.Science in China(Series D),1999,42(Suppl.1):80～90
[8]
郑卓,Guiot J.我围热带地区40万年以来古气候的定量恢复.中山大学学报(自然科学版),1999,38(6):94～98 Zheng Zhuo,Guiot J.A 400000-year paleoclimate reconstruction in tropical region of China.Acts Scientiarum Naturalium Universitatis Sunyatseni,1999,38(6):94～98
[9]
王乃昂,王涛,史正涛等.河西走廊术次冰期砂楔的发现及其古气候意义.冰川冻土,2001,23(1):46～50 Wang Nai''ang,Wang Tao,Shi Zhengtao et al.The discovery of sand wedges of the Last Glaciation in the Hexi Corridor and its paleoclimatic significance.Journal of Glaciology and Geocryology,2001,23(1):46～50
[10]
王会军,曾庆存.冰期气候的数值模拟.气象学报,1992,50(3):279～289 Wang Huijun,Zeng Qingcun.The numerical simulation of the ice age climate.Acta Meteorologica Sinica,1992,50(3):279～289
[11]
刘晓东,吴锡浩,董光荣等.末次冰期东亚季风气候的数值模拟研究.气象科学,1995,15(4):183～196 Liu Xiaodong,Wu Xihao,Dong Guangrong et al.A modeling research on East Asia monsoonal climate at the Last Glacial Maximum.Scientia Meteorologica Sinica,1995,15(4):183～196
[12]
钱云,钱永甫.18000年前冰期气候的数值模拟.地球物理学报,1998,41(6):752～762 Qian Yun,Qian Yongpu.The numerical simulation of the climate of 18000 years before present.Acta Geophysica Sinica,1998,41(6):752～762
[13]
钱云,钱永甫,张耀存.末次冰期东亚区域气候变化的情景和机制研究.大气科学,1998,22(3):283～293 Qian Yun,Qian Yongpu,Zhang Yaocun.Study on scenarios and mechanism of the regional climate change of East Asia in the last ice-age.Scientia Atmospherica Sinica,1998,22(3):283～293
[14]
陈星,于革,刘健.中国21 kaBP气候模拟的初步试验.湖泊科学,2000,12(2):154～164 Chen Xing,Yu Ge,Liu Jian.A preliminary simulation of climate at 21kaBP in China.Journal of Lake Sciences,2000,12(2):154～164
[15]
于革,陈星,刘健等.末次盛冰期东亚气候的模拟和诊断初探.科学通报,2000,45(20):2153～2159 Yu Ge,Chen Xing,Liu Jian et al.Preliminary study on LGM climate simulation and the diagnosis for East Asia.Chinese Science Bulletin,2001,46(5):364～368
[16]
姜大膀,王会军,郎咸梅.末次盛冰期气候模拟及青藏高原冰盖的可能影响.第四纪研究,2002,22(4):323～331 Jiang Dabang,Wang Huijun,Lang Xianmei.Palaeoclimate modeling for the LGM and the possible influence of the continental ice sheet over the Qinghai-Xizang Plateau.Quaternary Sciences,2002,22(4):323～331
[17]
Liu J,Yu G,Chen X.Palaeoclimate simulation of 21 kaBP for the Tibetan Plateau and Eastern Asia.Climate Dynamics,2002,19:575～583
[18]
郑益群,于革,王苏民等.区域气候模式对末次盛冰期东亚季风气候的模拟研究.中国科学(D辑),2002,32(10):871～880 Zheng Yiqun,Yu Ge,Wang Sumin et al.Simulations of LGM climate of East Asia by regional climate model.Science in China(Series D),2003,33(8):753～764
[19]
Jiang Dabang,Wang Huijun,Drange H et al.Last Glacial Maximum over China:Sensitivities of climate to paleovegetation and Tibetan ice sheet.Journal of Geophysical Research,2003,108(D3):4102,doi:10.1029/2002JD002167
[20]
Yu Ge,Xue Bin,Liu Jian et al.LGM lake records from China and an analysis of climate dynamics using a modelling approach.Global and Planetary Change,2003,38(3～4):223～256
[21]
赵平,陈隆勋,周秀骥等.末次盛冰期东亚气候的数值模拟.中国科学(D辑),2003,33(6):557～562 Zhao Ping,Chen Longxun,Zhou Xiuji et al.Modeling of the East Asian climate during the Last Glacial Maximum.Science in China(Series D),2003,46(10):1060～1068
[22]
Zhao Ping,Zhou Xiuji,Jian Zhimin et al.Modeling the tropical climate and the impact of the western Pacific sea surface temperature at the Last Glacial Maximum.Journal of Geophysical Research,2004,109:D08105,doi:10.1029/2003JD004095
[23]
隋伟辉,赵平.末次盛冰期西太平洋海温差异对亚洲夏季风影响的数值模拟.第四纪研究,2005,25(5):645～654 Sui Weihui,Zhao Ping.Modeling the impact of the western Pacific sea surface temperature difference on the Asian summer monsoon climate at the Last Glacial Maximum.Quaternary Sciences,2005,25(5):645～654
[24]
Zheng Y,Yu G,Wang S et al.Simulation of paleoclimate over East Asia at 6ka BP and 21 ka BP by a regional climate model.Climate Dynamics,2004,23(5):513～529
[25]
Ju Lixia,Wang Huijun,Jiang Dabang.Simulation of the Last Glacial Maximum climate over East Asis with a regional climate model nested in a general circulation model.Palaeogeography,Palaeoclimatology,Palaeoecology,2007,248(3～4):376～390
[26]
梁潇云,姜大膀.我国对末次冰期冰盛期尔亚区域古气候模拟的研究.气候变化研究进展,2007,3(3):138～143 Liang Xiaoyun,Jiang Dabang.Advances in East Asian paleoclimate modelling for the Last Glacial Maximum by China.Advances in Climate Change Research,2007,3(3):138～143
[27]
Pinot S,Ramstein G,Harrison S P et al.Tropical paleoclimates at the Last Glacial Maximum:Comparison of Paleoclimate Modeling Intercomparison Project(PMIP)simulations and paleodata.Climate Dynamics,1999,15:857～874
[28]
Zeng Qingcun,Yuan Chongguang,Zhang Xuehong et al.A global grid point general circulation model.In:Collection of Paper Presented at the WMO/IUGG NWP Symposium(Special volume of J.Meteorol.Soc.Japan),Tokyo,4～8 August 1986,1987.421～430
[29]
Zhang Xuehong.Dynamical framework of lAP nine-level atmospheric general circulation model.Advances in Atmospheric Sciences,1990,7(1):66～77
[30]
Liang Xiozhong.Description of a nine-level grid point atmospheric general circulation model.Advances in Atmospheric Sciences,1996,13(3):269～298
[31]
Jiang Dabang,Zhang Zbongshi.Paleoclimate modelling at the Institute of Atmospheric Physics,Chinese Academy of Sciences.Advances in Atmospheric Sciences,2006,23(6):1040～1049
[32]
Berger A L.Long-term variations of daily insolation and Quaternary climatic changes.Journal of the Atmospheric Sciences,1978,35(12):2362～2367
[33]
Pehier W R.Ice age paleotopography.Science,1994,265:195～201
[34]
Yu G,Chen X,Ni J et al.Palaeovegetation of China:A pollen databased synthesis for the mid-Holocene and last glacial maximum.Journal of Biogeography,2000,27(3):635～644
[35]
CLIMAP Project members.Seasonal reconstructions of the Earth''s surface at the Last Glacial Maximum.Geological Society of America Map and Chart Series MC-36.1981.1～18
[36]
Raynaud D,Jouzel J.Barnola J M et al.The ice record of greenhouse gases.Science,1993,259:926～934
[37]
Kalnay E,Kanamitsu M.Kistler R et al,The NCEP/NCAR 40-year reanalysis project.Bulletin of the American Meteorological Society,1996,77(3):437～471
[38]
Jiang Dabang,Wang Huijun,Ding Zhongli et al.Modeling the Middle Pliocene climate with a global atmospheric general circulation model.Journal of Geophysical Research,2005,110:D14107,doi:10.1029/2004JD005639
[39]
Wyputta U,McAvaney B J.Influence of vegetation changes during the Last Glacial Maximum using the BMRC atmospheric general circulation model.Climate Dynamics,2001,17(12):923～932
[40]
Xie P.Arkin P A.A 17-year monthly analysis based on gauge observations,satellite estimates,and numerical model outputs.Bulletin of the American Meteorological Society,1997,78:2539～2588
[41]
Tao S Y,Chen L X.A review of recent research on the East Asian monsoon in China.In:Chang C P.Krishnamurti T N.Monsoon Meteorology.New York:Oxford University Press,1987.60～92
[42]
Anderson D M,Webb R S.Ice-age tropics revised.Nature,1994,364:23～24
[43]
姚檀栋.末次冰期青藏高原的气候突变--古里雅冰芯与格陵兰GRIP冰芯对比研究.中国科学(D辑),1999,29(2):175～184 Yao Tandong.Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age--Comparative study of the Guliya ice core with the Greenland GRIP ice core.Science in China(Series D),1999,42(4):358～368
[44]
Farrera I,Harrison S P,Prentice I C et al.Tropical climates at the Last Glacial Maximum:A new synthesis of terrestrial palaeoclimate data.I.Vegetation,lake-levels and geochemistry.Climate Dynamics,1999,15:823～856
[45]
Mix A C,Morey A E,Pisias N G et al.Foraminiferal faunal estimates of paleotemperature:Circumventing the no-analog problem yields cool ice age tropics.Paleoceanography,1999,14(3):350～359
[46]
Wang P X.Response of western Pacific marginal seas to glacial cycles:Paleoceanographic and sedimentological features.Marine Geology,1999,156(1):5～39
[47]
Ding Z L,Liu T S,Rutter N W et al.Ice-volume forcing of East Asian winter monsoon variations in the past 800000 years.Quaternary Research,1995,44(2):149～159
[48]
丁仲礼,余志伟.第四纪时期东亚季风变化的动力机制.第四纪研究,1995,(1):63～74 Ding Zhongli,Yu Zhiwei.Forcing mechanisms of paleomonsoons over East Asia.Quaternary Sciences,1995,(1):63～74
[49]
Jin L Y,Ganopolski A,Chen F H et al.Impacts of snow and glaciers over Tibetan Plateau on Holocene climate change:Sensitivity experiments with a coupled model of intermediate complexity.Geophysical Research Letters,2005,32:L17709,doi:10.1029/2005GID23202
