[1] Kutzbach J E, Prell W L, Ruddiman W F. Sensitivity of Eurasian Climate to surface uplift of the Tibetan Plateau[J]. Journal of Geology,1993,101:177-190.
[2] 孙鸿烈, 郑度.青藏高原综合科学考察研究的回顾与展望[C]∥郑度等主编.青藏高原形成环境与发展. 石家庄: 河北科学技术出版社, 2003.
[3] Guo Z T, Ruddiman W, Hao Q Z, et al. Onset of Asian desertifications by 22Myr ago inferred from loess deposits in China[J]. Nature,2002,416:159-163.
[4] Fang X M, Carmala G, Rob V, et al. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin,China[J]. Earth and Planetary Science Letters,2003,210:545-560.
[5] Liu X D, Yin Z Y. Sensitivity of East Asian monsoon climate to the uplift of the Tibetan Plateau. Palaeogeography[J]. Palaeoclimatology, Palaeoecology,2002,183:223-245.
[6] 姚檀栋, 徐柏青, 段克勤, 等.青藏高原达索普冰芯2 ka来温度和甲烷浓度变化记录[J].中国科学:D辑,2002,32(4):346-352.
[7] Zhu Liping, Wang Junbo, Chen Ling, et al. 20,000-year environmental change reflected by Multidisciplinary Lake sediments in Chen Co, Southern Tibet[J]. Acta Geographica Sinica,2004,59(4):514-524.[朱立平,王君波,陈玲,等.藏南沉错湖泊沉积多指标揭示的二万年以来环境变化[J].地理学报,2004,59(4):514-524.]
[8] Thompson L G, Mosley-Thompson E, Davis M E, et al. Tropical glacier and ice core evidence of climate change on annual to millennial time scales[J]. Climatic Change,2002,59:137-155.
[9] 施雅风,刘时银.中国冰川对21世纪全球变暖响应的预估[J].科学通报,2000,45(4):434-438.
[10] Meier M F, Dyurgerov M B. How Alaska affects the world[J]. Science,2002,297:350-351.
[11] Wang S L, Niu F J, Zhao L, et al. The thermal stability of roadbed in permafrost regions along Qinghai-Tibet Highway[J]. Cold Regions Science and Technology,2003,37:25-34.
[12] Chen Guichen, Huang Zhiwei, Lu Xuefeng, et al. Characteristics of wetland and its conservation in the Qinghai Plateau[J]. Journal of Glaciology and Geocryology,2002,24(3):254-259.[陈桂琛, 黄志伟, 卢学峰, 等. 青海高原湿地特征及其保护[J].冰川冻土,2002,24(3):254-259.]
[13] Klein J A, Harte J, Zhao X Q. Experimental warming causes large and rapid species loss, dampened by simulated grazing, on the Tibetan Plateau[J]. Ecology Letters,2004,7(12):1 170-1 179.
[14] 郑度,姚檀栋,等.青藏高原隆升与环境效应[M]. 北京: 科学出版社,2004.
[15] Bollasina M, Benedict S. The role of the Himalayas and the Tibetan Plateau within the Asian monsoon system[J]. Bulletin of the American Meteorological Society,2004,85(7):1 001.
[16] Wu Guoxiong, Liu Yimin, Liu Xin, et al. How the heating over the Tibetan Plateau affects the Asian climate in summer[J]. Chinese Journal of Atmospheric Sciences,2005,29(1):47-56.[吴国雄, 刘屹岷, 刘新, 等.青藏高原加热如何影响亚洲夏季的气候格局[J]. 大气科学,2005,29(1):47-56.]
[17] 方小敏, 韩永翔, 马金辉, 等. 青藏高原沙尘特征与高原黄土堆积: 以2003-03-04拉萨沙尘天气过程为例[J]. 科学通报,2004,49(11):1 084-1 090.
[18] Wu T W, Qian Z G. The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall: An observational investigation[J]. Journal of Climate,2003,16:2 038-2 051.
[19] 苏珍, 施雅风. 小冰期以来中国季风温冰川对全球变暖的响应[J]. 冰川冻土,2000,22(3):223-229.
[20] Rea D K, Snoeckx H, Joseph L H. Late Cenozoic eolian deposition in the northern Pacific: Asian drying, Tibet uplift, and cooling of the northern hemisphere[J]. Palaeoceanography,1998,13:215-224.
[21] Raymo M E, Ruddiman W F, Froelich P N. Influence of late Cenozoic mountain building on ocean geochemical cycles[J]. Geology,1988,16:649-653.
[22] Moore III B. Meeting tomorrow's challenges[J]. IGBP News Letter,1999,38:2.
[23] Chen Yiyu, Chen Panqin, Ge Quansheng, et al. Global change research: Progress and prospect[J]. Earth Science Frontiers,2002,9(1):11-18.[陈宜瑜,陈泮勤,葛全胜,等.全球变化研究进展与展望[J]. 地学前缘,2002,9(1):11-18.]
|