JIA Yulian, SHI Yafeng, MA Chunmei, SHEN Hongyuan, WU Jinglu . Comparison of Palaeoclimatic Oscillations in Asian and African Monsoon Areas since 40 kaBP and Pan-lake Period of Tibetan Plateau[J]. Acta Geographica Sinica, 2004 , 59(6) : 829 -840 . DOI: 10.11821/xb200406004

[1] Li Bingyuan. The large lake period in the Tibet Plateau. Acta Geographica Sinica, 2000, 55(2): 174-181.
[李炳元. 青藏高原大湖期. 地理学报, 2000, 55(2): 174-181.]

[2] Shi Yafeng, Yu Ge, Liu Xiaodong et al. Reconstruction of the 40-30 kaBP enhanced India Monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169 (2): 69-83.

[3] Jia Yulian, Shi Yafeng, Wang Sumin et al. Lake expanding events in the Tibetan Plateau since 40 kaBP. Science in China, 2001, 44(suppl.): 301-315.

[4] Jia Yulian, Shi Yafeng, Fan Yunqi. Water balance of paleo-lake Qinghai and its precipitation estimation at three high lake-level stages since 40 kaBP. Journal of Lake Sciences, 2000, 12(3): 211-218.
[贾玉连, 施雅风, 范云崎. 四万年以来青海湖的三期高湖面及其降水量研究. 湖泊科学, 2000, 12(3): 211-218.]

[5] Jia Yulian, Shi Yafeng, Fan Yunqi et al. The precipitation of the interior lakes in the south-western Tibetan Plateau 40~30 kaBP. Advances in Earth Sciences, 2001, 6(4): 346-351.
[贾玉连, 施雅风, 曹建廷 等. 40-30kaBP期间高湖面稳定存在时期青藏高原西南部封闭流域的古降水量重建. 地球科学进展, 2001, 6(4): 346-351.]

[6] Shi Yafeng, Jia Yulian, Ge Yu et al. Features, impacts and causes of the high temperature and large precipitation event in the Tibetan Plateau and its adjacent area during 40-30 kaBP. Journal of Lake Sciences, 2002, 14(1): 1-11.
[施雅风, 贾玉连, 于革 等. 40-30kaBP青藏高原及邻区高温大降水事件的特征、影响及原因探讨. 湖泊科学, 2002, 14(1): 1-11.]

[7] Gao Youxi. Several Issues about Eastern Asia Monsoon. Beijing: Science Press, 1962. 27-35.

[8] Street F A. Global maps of lake-level fluctuations since 30,000 yr BP. Quaternary Research, 1979, 12(1): 83-118.

[9] Harrison S P. Late Quaternary lake-level record from Northern Eurasia. Quaternary Research, 1996, 45 (2): 138-159.

[10] Street F A, Grove A T. Environmental and climatic implications of the late Quaternary lake level fluctuations in Africa. Nature, 1976, 261: 385-390.

[11] Yu Ge. Studies of global late Quaternary lake-level data bases. Journal of Lake Sciences, 1997, 9(3): 193-202.
[于革. 全球晚第四纪湖泊数据库的研究. 湖泊科学, 1997, 9(3): 193-202.]

[12] Tarasov P E, Harrison S P, Saarse L et al. Lake status records from the former Soviet Union and Mongolia. NOAA Paleoclimatology Publications Series Report, 1994, 2: 1-274.

[13] An Z S, Kukla G J, Porter S C et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quaternary Research, 1991, 36(1): 29-36.

[14] Lv Houyuan, Han Jiamao, Wu Naiqin et al. Modern Soil Magnetic susceptibility in China and its paleoclimatic implications. Science in China (B), 1994, 24(12): 1290-1297.
[吕厚远, 韩家懋, 吴乃琴 等. 中国现代土壤磁化率分析及其古气候意义. 中国科学 (B), 1994, 24(12): 1290-1297]

[15] Maher B A, Thompson R, Zhou L P. Spatial and temporal reconstruction of changes in the Asian Monsoon: a new mineral magnetic approach. Earth Planet Sci. Lett., 1994, 125(4): 461-471.

[16] Ding Zhongli, Ren Jianzhang, Liu Dongsheng et al. Millennial-scale irregular change of monsoon-desert system during late Pleistocene and its causes. Science in China (D), 1996, 26(5): 385-391.
[丁仲礼, 任剑璋, 刘东生 等. 晚更新世季风—沙漠系统千年尺度的不规则变化及其机制问题. 中国科学(D), 1996, 26(5): 385-391.]

[17] Nie Gaozhong, Liu Jiaqi, Guo Zhengtang. The important stratum boundaries since 150 kaBP in Weinan loess profile, and their climate events: chronological proofs. Quaternary Sciences, 1996, 3: 202-210.
[聂高众, 刘嘉麒, 郭正堂. 渭南黄土剖面十五万年以来的主要地层界线和气候事件. 第四纪研究, 1996, 3: 202-210.]

[18] Guo Zhengtang, Pen Shuzhen, Wei Lanying et al. Millennial-scale oscillations of eastern summer monsoon over the last 0.22Ma. Quaternary Sciences, 1999, (4): 299-305.
[郭正堂, 彭淑贞, 魏兰英 等. 二十二万年以来东亚夏季风的千年尺度变化及其在不同时期的差异. 第四纪研究, 1999, (4): 299-305.]

[19] Gasse F. Evolution of lake Abhe (Ethiopia and TFAI) from 70,000 aBP. Nature, 1977, 265: 42-45.

[20] Gasse F, Ledee V, Massault M et al. Water-level fluctuations of lake Tanganyika in phase with oceanic changes during the last glaciation and deglaciation. Nature, 1989, 342: 57-59.

[21] Bonnefile R, Riollet G. The Kashiru pollen sequence (Burundi), paleoclimatic implications for the last 40,000 yr BP in tropical Africa. Quaternary Research, 1988, 30(1): 19-35.

[22] Bonnefille R, Roeland J C, Guiot J. Temperature and rainfall estimates for the past 40,000 yr BP in Equatorial East Africa. Nature, 1990, 346: 347-349.

[23] Aucour A M, Hillaire-Marcel C, Bonnefille R. Late Quaternary biomass changes from 13C measurements in a highland peatbog from Equatorial Africa (Burundi). Quaternary Research, 1994, 41(2): 225-233.

[24] Taylor M D. Late Quaternary pollen records from two Ugandan mires: evidence for environmental change in the Rukiga highlands of southwest Uganda. Palaogeography, Palaeoclimatology, Palaeoecology, 1990, 80(2): 283-300.

[25] Butzer K W, Isaac G L. Radiocarbon dating of East African lake levels. Science, 1972, 175: 1069-1076.

[26] Richardson J L. Palaeolimnological records from rift lakes in central Kenya. Palaeoecology of Africa, 1972, 11(4): 131-138.

[27] Durand A. Oscillations of lake Chad over the past 50,000 years: new data and new hypothesis. Palaeogeography, 1982, 39(1): 37-53.

[28] Wendorf F. The members of the Combined Prehistoric Expedition. Late Pleistocene and recent climatic changes in the Egyptian Sahara. Geographical Journal, 1977, 143(2): 211-234.

[29] Foucault A, Stanley D J. Late Quaternary palaeocliamtic oscillations in East Africa recorded by heavy minerals in the Nile delta. Nature, 1989, 339: 44-46.

[30] Zheng Mianping, Xiang Jun. Salt Lakes in the Tibetan Plateau. Beijing: Geology Press, 1989. 1-353.

[31] Qi Wen, Zheng Mianping. Sedimentary features and climate evolution from ZK91-2 core in Zhabyer Caka, in the Tibetan Plateau. Journal of Lake Sciences, 1995, 7(2): 133-140.
[齐文, 郑绵平. 西藏扎布耶湖ZK91-2钻孔沉积特征与气候演化. 湖泊科学, 1995, 7(2): 133-140.]

[32] Xiao Jiayi, Wu Yushu, Zheng Mianping. Preliminary studies of late Quaternary pollen flora in Zhabyer Caka, in the Tibetan Plateau. Acta Micropaleontologica Sinica, 1996, 13(4): 395-399.
[萧家仪, 吴玉书, 郑绵平. 西藏扎布耶盐湖晚第四纪孢粉植物群的初步研究. 微体古生物学报, 1996, 13(4): 395-399.]

[33] Bhattacharyya A. Vegetation and climate during the last 30,000 years in Ladakh. Palaeogeography, Palaeoclimatology, Palaeoecology, 1989, 73(1): 25-38.

[34] Li Shijie, Li Bingyuan, Zhu Zhaoyu et al. Lake sediment records of Tianshuihai core. In: Shi Yafeng, Li Jijun, Li Bingyuan (eds.), Late Quaternary Uplifting and Environmental Evolution in the Tibetan Plateau. Guangzhou: Guangdong Science and Technology Press, 1998. 215-246.

[35] Zhang Pengxi, Zhang Baozhen, Wenluositan T K et al. Causes of Formation of the Paleopotansium Salt and Paleotranspiration Salt: A Case Study of Salt Lake in Qaidam Basin. Beijing: Science Press, 1993. 84-99.

[36] Chen Kezao, Bowler J M, Kelts K. Climate change in the Tibetan Plateau since 40 kaBP. Quaternary Sciences, 1990, 10 (1): 21-31.
[陈克造, Bowler J M, Kelts K. 四万年来青藏高原的气候变迁. 第四纪研究, 1990, 10(1): 21-31.]

[37] Huang Qi. Dating of several salt lake ages and their sediment cycles. Chinese Science Bulletin, 1980, 25(21): 990-994.
[黄麒. 盐湖年龄的测定——青藏高原几个盐湖的14C年龄及其沉积旋回. 科学通报, 1980, 25(21): 990-994.]

[38] Huang Qi. Model of paleoclimate change in dry area reconstructed by organic geochemistry method. Oceanologia end Limnologia Sinica, 1991, 22(3): 547-553.
[黄麒. 干旱地区古气候变化特征. 海洋与湖沼, 1991, 22(3): 547-553.]

[39] Pachur H J, Wunnemann B, Zhang H C. Lake evolution in the Tengger desert, northwestern China, during the last 40,000 years. Quaternary Research, 1995, 44(2): 171-180.

[40] Yuan Baoyin, Chen Kezao, Bowler J M et al. Formation and evolution of Qinghai Lake. Quaternary Sciences, 1990, 10(3): 233-243.
[袁宝印, 陈克造, Bowler J M 等. 青海湖的形成与演化趋势. 第四纪研究, 1990, 10(3): 233-243.]

[41] Shan Fashou, Du Naiqiu, Kong Zhaochen. Vegetable evolution and environmental change in Qinghai Lake basin at the last 350 kaBP. Journal of Lake Sciences, 1993, 5(1): 9-17.
[山发寿, 杜乃秋, 孔昭宸. 青海湖盆地35万年来植被演化与环境变迁. 湖泊科学, 1993, 5(1): 9-17.]

[42] Lister G S, Kelts K, Zao C K et al. Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene. Palaogeography, Palaeoclimatology, Palaeoecology, 1991, 84(1): 141-162.

[43] Lanzhou Subacademy of Chinese Academy of Sciences, Research Center of Western Resource and Environment of Chinese Academy of Sciences. Evolution of Recent Environment of Qinghai Lake and Prognostication for the Future. Beijing: Science Press, 1994. 1-79.

[44] Pan Baotian, Wang Jianmin. Loess record of Qingzang Plateau monsoon variations in the eastern part of Qingzang Plateau since in the last interglacial. Quaternary Sciences, 1999, 19(4): 330-334.
[潘保田, 王建民. 末次间冰期以来青藏高原东部季风演化的黄土沉积记录. 第四纪研究, 1999, 19(4): 330-334.]

[45] Le Heling, Dong Guangrong, Gao Shangyu et al. Environmental and south-western monsoon variations in central Tibetan Plateau since 300 kaBP. Journal of Desert Research, 2000, 20(3): 234-236.
[靳鹤龄, 董光荣, 高尚玉 等. 距今30万年来西藏中部地区环境变化与西南季风变迁. 中国沙漠, 2000, 20(3): 234-236.]

[46] Yan Shun, Mu Guijin et al. Quaternary environmental evolution of the Lop Nur region, China. Acta Geographica Sinica, 1998, 53(4): 332-340.
[闫顺, 穆桂金 等. 新疆罗布泊地区第四纪环境演变. 地理学报, 1998, 53(4): 332-340.]

[47] Li Bingyuan, Cai Biqin. Sedimentary feature of Aiding Lake in Tulufan Basin. Chinese Science Bulletin, 1989, 34(8): 608-610.
[李秉孝, 蔡碧琴. 吐鲁番盆地艾丁湖沉积特征. 科学通报, 1989, 34(8): 608-610.]

[48] Shi Yafeng, Wen Qizhong. Quaternary climate change and hydrogeological change in Caiwobao Lake, Xinjiang. Beijing: Science Press, 1990. 147-157.

[49] Rhodes T E, Gasse F, Lin R F et al. A late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China). Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 120: 105-125.

[50] Lin Ruifen. Paleoclimtic and paleoenvironmental change from Manasi Lake core, Xinjiang. J. of Geochemistry, 1996, 25(1): 63-71.
[林瑞芬. 新疆玛纳斯湖沉积柱样的古气候古环境研究. 地球化学, 1996, 25(1): 63-71.]

[51] Han Shuti, Yuan Yujiang. The sequence of paleoclimatic variation of Balikun Lake of Xinjiang in the past 35000 years. Acta Geographica Sinica, 1990, 45(3): 350-362.
[韩淑缇, 袁玉江. 新疆巴里坤湖35000 年来古气候变化序列. 地理学报, 1990, 45(3): 350-362.]

[52] Yuan Baoyin. Paleohydrological evolution of Balikun Lake, Xinjiang, since 150 kaBP. Quaternary Sciences, 1998, (4): 319-327.
[袁宝印. 新疆巴里坤湖十五万年来古水文演化序列. 第四纪研究, 1998, (4): 319-327.]

[53] Yin Yong, Fang Nianqiao. Lacustrine records of environment change during the last 57ka in Panahai lake, in northwestern of Yunnan, China. Marine Geology and Quaternary Geology, 2002, 22(4): 99-105.
[殷勇, 方念乔. 云南中甸纳帕海湖泊沉积记录指示的57ka环境变化. 海洋地质与第四纪地质, 2002, 22(4): 99-105.]

[54] Hodell D A, Brenner M, Kanfoush S L et al. Paleoclimate of southwestern China for the past 50,000 yr inferred from lake sediment records. Quaternary Research, 1999, 52(3): 369-380.

[55] Shi Ying, Tong Guobang, Wang Sumin et al. Late Quaternary diatom community and environment changes in Heqing Basin, Yunnan. Marine Geology and Quaternary Geology, 1998, 18(4): 79-85.
[石英, 童国榜, 王苏民 等. 云南鹤庆盆地晚第四纪硅藻植物群与环境. 海洋地质与第四纪地质, 1998, 18(4): 79-85.]

[56] Peng Jinlan. Ostracodes of the Heqing Basin, Yunnan and environmental changes during the last 150000 yr. J. of Lake Sciences, 2003, 15(1):1-10.
[彭金兰. 云南鹤庆盆地15万年以来的介形类及环境演变. 湖泊科学, 2003, 15(1): 1-10.]

[57] Yang Xidong, Wang Sumin, Tong Guobang et al. Late Pleistocene pollen records and paleoclimate implications in Heqing Paleolake, Yunnan. Quaternary Sciences, 1998, 18(4): 335-341.
[羊向东, 王苏民, 童国榜 等. 云南鹤庆古湖晚更新世的孢粉记录及其古气候意义. 第四纪研究, 1998, 18(4): 335-341.]

[58] Tang Lingyu. Vegetation history and their paleoclimatic implication since 40kaBP, in Menghai region, Yunnan. Acta Micropalaeontologica Sinica, 1992, 9(4): 433-455.
[唐领余. 云南勐海地区四万年以来植被史与古气候意义. 微体古生物学报, 1992, 9(4): 433-455.]

[59] Xiao Jiayi. Paleovegetational and paleoenvironmental changes in Kunming region, Yunnan. Journal of Southeastern Culture, 1992, (4): 56-62.
[萧家仪. 云南昆明地区5万年以来的古植被与古环境演变. 东南文化, 1992, (4): 56-62.]

[60] Sun Donghuai, Zhou Jie, Jiang Fuchu et al. Preliminary studies on Chinese Loess Plateau summer monsoon change during the last interglacial. Chinese Science Bulletin, 1996, 40(20): 1873-1875.
[孙东怀, 周杰, 蒋复出 等. 末次间冰期黄土高原夏季风气候的初步研究. 科学通报, 1996, 40(20): 1873-1875.]

[61] Li Yumei, Liu Dongsheng, Wu Wenxiang et al. Warm and moist paleoclimate during MIS3 recorded by Malan Loess in Chinese Loess Plateau. Quaternary Sciences, 2003, 23(1): 69-76.
[李玉梅, 刘东生, 吴文祥 等. 黄土高原马兰黄土记录的MIS3温湿气候. 第四纪研究, 2003, 23(1): 69-76.]

[62] An Z S, KG J, Porter S C et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau. Quaternary Research, 1991, 36(1): 29-36.

[63] Wu Xihao, Jiang Fuchu, Xiao Huaguo et al. Structure movement and climate change at the last 200 ka recorded by Mangshan loess at the central part of China. Science in China (D), 1999, 29(1): 76-81.
[吴锡浩, 蒋复初, 肖华国 等. 中原邙山黄土及最近200ka构造运动与气候变化(OSL). 中国科学(D), 1999, 29(1): 76-81.]

[64] Li Jijun, Zhu Junjie, Kang Jiancheng et al. Comparison of the last glacial cycle recorded Lanzhou loess profile and ice core from Eastern Station of South Pole. Science in China (B), 1990, 20(10): 1086-1094.
[李吉均, 朱俊杰, 康建成 等. 末次冰期旋回兰州黄土剖面与南极东方站冰芯的对比. 中国科学(B), 1990, 20(10): 1086-1094.]

[65] Chen F H, Bloemendal J, Wang J M et al. High-resolution multi-proxy climate records from Chinese loess: evidence for rapid climatic changes over the last 75kyr. Palaeogeography, Palaeoclimatology, Palaeoecology, 1997, 130: 323-335.

[66] Fang Xiaomin, Pan Baotian, Guan Donghong et al. Millennial-scale instability studies of summer monsoon during ca 60 kaBP recorded Lanzhou loess profile. Chinese Science Bulletin, 1999, 44(4): 436-439.
[方小敏, 潘保田, 管东红 等. 兰州约60kaBP以来夏季风千年尺度不稳定性研究. 科学通报, 1999, 44(4): 436-439.]

[67] Sun Jimin, Ding Zhongli, Liu Dongsheng et al. Environmental changes in the desert-loess transitional zone of north China since the beginning of the last interglacial. Quaternary Sciences, 1995, 15(2): 117-122.
[孙继敏, 丁仲礼, 刘东生 等. 末次间冰期以来沙漠-黄土边界带的环境演变. 第四纪研究, 1995, 15(2): 117-122.]

[68] Ding Zhouli, Sun Jimin. Paleoclimatic events in Chinese Loess Plateau during the last 130kaBP. Chinese Science Bulletin, 1998, 43(6): 567-574.
[仲礼, 孙继敏. 黄土高原过去130ka来古气候事件. 科学通报, 1998, 43(6): 567-574.]

[69] Gao Quanzhou, Tao Zhen, Dong Guangrong et al. The characteristics of sediments geochemistry in Chagelebulu section in the Badain Jaran Desert. Acta Geographica Sinica, 1998, 53(suppl.): 44-52.
[高全洲, 陶贞, 董光荣 等. 巴丹吉林沙漠查格勒布鲁剖面的沉积地球化学特征. 地理学报, 1998, 53(增刊): 44-52.]

[70] Zhang Hucai. A study on loess sedimentation and environmental change since late Pleistocene in Wudu area. Journal of Lanzhou University (Natural Sciences), 1997, 33(1): 105-114.
[张虎才. 武都黄土堆积及晚更新世以来环境变迁研究. 兰州大学学报, 1997, 33(1): 105-114.]

[71] Lu Huayu. Climatic change during the last 130kaBP recorded by Xining loess profile. Quaternary Sciences, 2001, 21(5): 416-426.
[鹿化煜. 西宁黄土堆积记录的最近13万年高原气候变化. 第四纪研究, 2001, 21(5): 416-426.]

[72] Yue L P, Lei X Y, Que H J. A magnetostratigraphic study on the Jingyuan loess section, Gansu, China. Quaternary Science Review, 1991, 10(4): 349-353.

[73] Sun Donghuai, An Zhisheng, Wu Xihao et al. Evolution of summer monsoon climatic pattern in Chinese Loess Plateau during the last 150kaBP. Science in China (D), 1996, 26(5): 417-422.
[孙东怀, 安芷生, 吴锡浩 等. 最近150ka黄土高原夏季风气候格局的演化. 中国科学 (D), 1996, 26(5): 417-422.]

[74] DeMenocal P B. Plio-Pleistocene African climate. Science, 1995, 270: 53-59.

[75] Jahns S, Huls M, Sarnthein M. Vegetation and climate history of west equatorial Africa based on a marine pollen record off Liberia covering the last 400,000 years. Review of Palaeobotany and Palynology, 1998, 102(2): 277-288.

[76] Petit-Maire N, Fontugne M, Rouland C. Atmospheric methane ratio and environmental changes in the Sahara and Sahel during the last 130 kyrs. Palaeogeography, Palaeoclimatology, Palaeoecology, 1991, 86(2): 197-204.

[77] Shi N, Dupont L M. Vegatational and climatic history of SW Africa: a marine palynological record of the last 300,000 years. Veg Hist Archaeobot, 1997, 34(6): 117-131.

[78] Prell W L, Campo E V. Coherent response of Arabian Sea upwelling and pollen transport to late Quaternary monsoonal winds. Nature, 1986, 323: 526-528.

[79] Emeis K C, Anderson D M, Doose H et al. Sea-surface temperatures and the history of monsoon upwelling in the Northwest Arabian Sea during the last 500,000 years. Quaternary Research, 1995, 43(3): 355-361.

[80] Van Campo E, Duplessy J C, Rossignol-Strick M. Climatic conditions deduced from a 150-kyr oxygen isotope-pollen record from the Arabian Sea. Nature, 1982, 296: 56-59.

[81] Schulz H, Rad von U, Erlenkeuser H. Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature, 1998: 54-57.

[82] Clemens S, Prell W, Murray D et al. Forcing mechanisms of the Indian Ocean monsoon. Nature, 1991, 353: 721-725.

[83] Prell W L. Monsoon variability over the past 150,000 years. J. of Geophysical Research, 1987, 92(D7): 8411-8425.

[84] Wang Sumin, Feng Min. Relationship between environmental change of Daihai Lake, Inner Mongolia, and Southeast Monsoon. Science in China (B), 1991, 21(7): 756-768.
[王苏民, 冯敏. 内蒙古岱海湖泊环境变化与东南季风强弱的关系. 中国科学(B), 1991, 21(7): 756-768.]

[85] McClure H A. Radiocarbon chronology of late Quaternary lakes in the Arabian Desert. Nature, 1976, 263: 755-756.

[86] Ding Z L, Liu T S, Rutter N W et al. Ice-volume forcing of East Asian Winter Monsoon variations in the past 800, 000 years. Quaternary Research, 1995, 44(2): 149-159.

[87] Ding Z L. Toward an orbital time scale for Chinese loess deposits. Quaternary Science Review, 1994, 13: 39-70.

[88] Wang Pinxian, Tian Jun. Quaternary glacial cycle shifting recorded in South China Sea. Science in China (D), 2001, 31(10): 793-799.
[汪品先, 田军. 第四纪冰期旋回转型在南沙深海的记录. 中国科学(D), 2001, 31(10): 793-799.]

[89] Clemens S, Prell W, Murray D et al. Nonstationary phase of Indian monsoon. Science, 1996, 274: 943-948.

[90] Berger A. Long-term variations of caloric insolation resulting from the Earth's orbital elements. Quaternary Research, 1978, 9: 139-167.

[91] Thompson L G, Yao T, Davis M E et al. Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science, 1997, 276: 1821-1825.

[92] Flohn H. Contributions to a Meyeorolgy of the Tibetan Highlands. Atmos. Sci. Paper, 1968, 130, Corolado State Univ. Ft. Collins.

[93] Wake C P, Mayewski P A, Qin A H et al. Changes in atmospheric circulation over the south-eastern Tibetan Plateau over the last two centuries: a Himalayan ice core. Pages News, 2001, 99(3): 11-13.

[94] Grosswald M G. Late Weichselian ice sheet of Northern Eurasia. Quaternary Research, 1980, 13(1): 1-32.

[95] Loewe F. Considerations on the origin of the Quaternary ice sheet of North America. Arctic and Alpine Research, 1971, 3: 331-344.

[96] Winograd I J. The magnitude and proximate cause ice sheet growth since 35,000 yr BP. Quaternary Research, 2001, 56: 299-307.