1 Barsugli J J, Sardeshmukh P D.Global atmospheric sensitivity to tropical SST anomalies throughout the Indo-Pacific Basin. Journal of Climate,2002, 15 :3427~3442
[2]
2 Yin, J H,Battisti D S.The importance of tropical sea surface temperature patterns in simulations of Last Glacial Maximum climate. Journal of Climate,2001, 14 :565~581
[3]
3 CLIMAP Project Members. Seasonal reconstruction of the Earth''s surface at the Last Glacial Maximum,Map and Chart Series MC-36.Geological Society of America,1981.1~18
[4]
4 MARGO Project Members. Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum. Nature Geoscience,2009, 2 : 127~132,doi: 10.1038/ngeo411
[5]
5 Toracinta E R, Oglesby R J,Bromwich D H.Atmospheric response to modified CLIMAP ocean boundary conditions during the Last Glacial Maximum. Journal of Climate,2004, 17 :504~522
[6]
6 Hostetler S, Pisias N,Mix A.Sensitivity of Last Glacial Maximum climate to uncertainties in tropical and subtropical ocean temperatures. Quaternary Science Reviews,2006, 25 :1168~1185
[7]
7 Hostetler S W, Mix A C.Reassessment of ice-age cooling of the tropical ocean and atmosphere. Nature,1999, 399 :673~676
[8]
8 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
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
Wang Yue,Jian Zhimin,Zhao Ping.Sensitivity of equatorial Pacific Convergence Zone to revised tropical sea surface temperature outside the warm pool during the Last Glacial Maximum. Quaternary Sciences,2009, 29 (2):221~231
[13]
11 Zheng W, Braconnot P,Guilyardi E et al.ENSO at 6ka and 21ka from ocean-atmosphere coupled model simulations. Climate Dynamic,2007, 30 :745~762
[14]
12 Wang Bin, Ding Qinghua,Fu Xiouhua et al.Fundamental challenges in simulation and prediction of summer monsoon rainfall.Geophysical Research Letters,2005, 32 : L15711,doi: 10.1029/2005GL02273412
Li Li,Wang Hui,Li Jianru et al.Variability of sea surface residual oxygen isotopic and salinity in Western South China Sea over Late Pleistocene. Quaternary Sciences,2008, 28 (3):399~406
[17]
26 Stott L, Timmermann A,Thunell R.Southern Hemisphere and deep-sea warming led deglacial atmospheric CO2 rise and tropical warming. Science,2007, 318 :435~438
[18]
27 Locarnini R A, Mishonov A V,Antonov J I et al.World Ocean Atlas 2005,Volume 1: Temperature.In: Levitus S ed.NOAA Atlas NESDIS 61,U.S.Washington,D.C.:Government Printing Office,2006.182
[19]
28 Wang L, Sarnthein M,Erlenkeuser H et al.East-Asian monsoon climate during the Late Pleistocene: High-resolution sediment records from the South China Sea. Marine Geology,1999, 156 (1~4):245~284
He Juan,Zhao Meixun,Li Li et al.Sea surface temperature and terrestrial biomarker records of the last 260ka of core MD05-2904 from the Northern South China Sea. Chinese Science Bulletin,2008, 53 (15):2376~2384
13 Wang Bin. Thrusts and prospects on understanding and predicting Asian monsoon climate. Acta Meteorologica Sinica,2008, 22 (4):383~403
[24]
14 Weinelt M, MARGO SST.Compilation of global planktic foraminifera LGM SST data. PANGAEA,2004,doi: 10.1594/PANGAEA.227620
[25]
15 Otto-Bliesner B L, Brady E C,Clauzet G et al.Last Glacial Maximum and Holocene climate in CCSM 3. Journal of Climate,2006, 19 :2526~2544
[26]
16 Collins W D, Rasch P J,Boville B A et al.Description of the NCAR Community Atmosphere Model(CAM 3.0). NCAR Technicl Note NCAR/TN-464+STR,2004.226
[27]
17 Kucera M, Weinelt M,Kiefer T et al.Reconstruction of sea-surface temperatures from assemblages of planktonic foraminifera: Multi-technique approach based on geographically constrained calibration data sets and its application to glacial Atlantic and Pacific Oceans. Quaternary Science Reviews,2005, 24 :951~998
[28]
18 Li C. A general circulation modeling perspective on abrupt climate change during glacial times.Washington: Ph.D thesis of Department of Atmospheric Sciences,University of Washington,2007.86
[29]
19 Braconnot P, Otto-Bliesner B,Harrison S et al.Results of PMIP 2 coupled simulations of the Mid-Holocene and Last Glacial Maximum-Part 2: Feedbacks with emphasis on the location of the ITCZ and mid-and high-latitudes heat budget. Climate of the Past,2007, 3 :279~296
[30]
20 Rind D, Peteet D.Terrestrial conditions and the Last Glacial Maximum and CLIMAP sea-surface temperature estimates: Are they consistent？Quaternary Research,1985, 24 :1~22
[31]
21 Schmidt G A, Bigg G R,Rohling E J.Global seawater oxygen-18 database.1999,http://data.giss.nasa.gov/o18data/
[32]
22 Bemis B E, Spero H J,Bijma J et al.Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations. Paleoceanography,1998, 13 (2):150~160
[33]
23 Waelbroeck C, Labeyrie L,Michel E et al.Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews,2002, 21 :295~305
[34]
24 de Garidel-Thoron T, Rosenthal Y,Beaufort L et al.A multiproxy assessment of the western equatorial Pacific hydrography during the last 30 kyr. Paleoceanography,2007, 22 :PA3204,doi: 10.1029/2006PA001269
[35]
Ge Huangmin,Li Qianyu,Cheng Xinrong et al.Late Quaternary high resolution monsoon records in planktonic stable isotopes from Northern South China Sea. Earth Science——Journal of China University of Geosciences,2010, 35 (4):515~525
[36]
31 Wei Ganjian, Deng Wenfeng,Liu Ying et al.High-resolution sea surface temperature records derived from foraminiferal Mg/Ca ratios during the last 260ka in the Northern South China Sea. Palaeogeography,Palaeoclimatology,Palaeoecology,2007, 250 :126~138
[37]
32 Büehring C, Sarnthein M,Erlenkeuser H.Toward a high resolution stable isotope stratigraphy of the last 1.1 million years,ODP Site 1144,South China Sea.In: Prell W L,Wang P,Blum P eds.Proceedings of the Ocean Drilling Program,Scientific Results,184 .2004.http://www-odp.tamu.edu/publications/184_SR/205/205.htm
[38]
33 Oppo D W, Sun Youbin.Amplitude and timing of sea-surface temperature change in the Northern South China Sea: Dynamic link to the East Asian monsoon. Geology,2005, 33 (10):785~788
[39]
34 Clemens S C, Prell W L,Sun Youbin et al.Southern Hemisphere forcing of Pliocene δ18 O and the evolution of Indo-Asian monsoons. Paleoceanography,2008, 23 : PA4210,doi: 10.1029/2008PA001638
Jian Zhimin,Wang Boshi,Qiao Peijun.Late Quaternary changes of sea surface temperature in the Southern South China Sea and their comparison with the paleoclimatic records of polar ice cores. Quaternary Sciences,2008, 28 (3):391~398
[42]
36 Steinke S, Chiu Hanyi,Yu Paisen et al.On the influence of sea level and monsoon climate on the Southern South China Sea freshwater budget over the last 22,000 years. Quaternary Science Reviews,2005, 25 (13~14):1475~1488
[43]
37 Steinke S, Kienast M,Groeneveld J et al.Proxy dependence of the temporal pattern of deglacial warming in the tropical South China Sea: Toward resolving seasonality. Quaternary Science Reviews,2008, 27 :688~700
[44]
38 Rosenthal Y, Oppo D W,Linsley B K.The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea,western equatorial Pacific. Geophysical Research Letters,2003, 30 (8): 1428,doi: 10.1029/2002GL016612.2003
[45]
39 Stott L, Poulsen C,Lund S et al.Super ENSO and global climate oscillations at millennial time scales. Science,2002, 297 :222~226
[46]
40 Visser K, Thunell R,Stott L.Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature,2003, 421 :152~155
[47]
41 Xu Jian, Holbourn A,Kuhnt W et al.Changes in the thermocline structure of the Indonesian outflow during Terminations I and II. Earth and Planetary Science Letters,2008, 273 :152~162
[48]
42 de Garidel-Thoron T, Rosenthal Y,Beaufort L et al.A multiproxy assessment of the western equatorial Pacific hydrography during the last 30 kyr. Paleoceanography,2007, 22 : PA3204,doi: 10.1029/2006PA001269
[49]
43 de Garidel-Thoron T, Rosenthal Y,Bassinot F et al.Stable sea surface temperatures in the Western Pacific warm pool over the past 1.75 million years. Nature,2005, 433 :294~298
[50]
44 Lea D W, Pak D K,Spero H J.Climate impact of Late Quaternary equatorial Pacific sea surface temperature variations. Science,2000, 289 :1719~1724
[51]
45 Leduc G, Vidal L,Tachikawa K et al.Moisture transport across Central America as a positive feedback on abrupt climatic changes. Nature,2007, 445 :908~911
[52]
46 Benway H M, Mix A C,Haley B A et al.Eastern Pacific Warm Pool paleosalinity and climate variability: 0~30kyr. Paleoceanography,2006, 21 : PA3008,doi: 10.1029/2005PA001208
[53]
47 Lea D W, Pak D K,Belanger C L et al.Paleoclimate history of Galagos surface waters over the last 135,000 yr. Quaternary Science Reviews,2006, 25 (11~12):1152~1167
[54]
48 Koutavas A, Lynch-Stieglitz J,Marchitto Jr T M et al. El Ni？o -like pattern in ice age tropical Pacific sea surface temperature. Science,2002, 297 :226~230
[55]
49 Rühlemann C, Mulitza S,Müeller P J et al.Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation. Nature,1999, 402 :511~514
[56]
50 Schmidt M W, Spero H J,Lea D W.Links between salinity variation in the Caribbean and North Atlantic thermohaline circulation. Nature,2004, 428 :160~163.
