2 Zhou T J, Zhang L X, Li H M. Changes in global land monsoon area and total rainfall accumulation over the last half century. Geophys Res Lett, 2008, 35: L16707, doi: 10.1029/2008GL034881
[2]
6 Wang B, Ding Q H. Changes in global monsoon precipitation over the past 56 years. Geophys Res Lett, 2006, 33: L06711, doi: 10.1029/2005GL025347
[3]
7 Chen H, Sun J. How large precipitation changes over global monsoon regions by CMIP5 models? Atmos Oceanic Sci Lett, 2013, 6: 306-311
[4]
10 Yu G, Xue B, Liu J, et al. LGM lake records from China and an analysis of climate dynamics using a modelling approach. Glob Planet Change, 2003, 38: 223-256
[5]
11 Chen F H, Wu W, Zhu Y, et al. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China. Chin Sci Bull, 2003, 48: 1401-1410 [陈发虎, 吴薇, 朱艳, 等. 阿拉善高原中全新世干旱事件的湖泊记录研究. 科学通报, 2004, 49: 1-
[6]
12 Yuan D, Cheng H, Edwards R L, et al. Timing, duration, and transitions of the last interglacial Asian monsoon. Science, 2004, 304: 575-578
[7]
13 Wang Y, Cheng H, Edwards R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224000 years. Nature, 2008, 451: 1090-1093
[8]
22 Zhou B T, Zhao P. Coupled simulation result of seasonal evolution of southwesterly wind climate over eastern China in mid-Holocene (in Chinese). Quat Sci, 2009, 29: 211-220 [周波涛, 赵平. 中全新世时期我国西南风气候季节演变的数值模拟结果分析. 第四纪研究, 2009, 29: 211-
[9]
24 Zhou B T, Zhao P. Modeling variations of summer upper tropospheric temperature and associated climate over the Asian Pacific region during the mid-Holocene. J Geophys Res, 2010, 115: D20109, doi: 10.1029/2010JD014029
[10]
25 Jiang D, Lang X, Tian Z, et al. Mid-Holocene East Asian summer monsoon strengthening: Insights from Paleoclimate Modeling Intercomparison Project (PMIP) simulations. Paleogeogr Paleoclimatol Paleoecol, 2013, 369: 422-429
[11]
26 Zhao P, Zhou X J, Jian Z M, et al. Modeling the tropical climate and the impact of the western Pacific sea surface temperature at the last glacial maximum. J Geophys Res, 2004, 109: D08105, doi: 10.1029/2003JD004095
[12]
27 Jiang D, Lang X. Last glacial maximum East Asian monsoon: Results of PMIP simulations. J Clim, 2010, 23: 5030-5038
[13]
28 Joussaume S, Taylor K E. Status of the Paleoclimate Modeling Intercomparison Project (PMIP). In: Gates W L, ed. Proceedings of the First International AMIP Scientific Conference: Monterey, California, USA, 15-19 May 1995. Geneva: World Meteorol Org, 1995. 425-430
[14]
32 Webster P J, Magana V O, Palmer T, et al. Monsoons: Processes, predictability, and the prospects for prediction. J Geophys Res, 1998, 103: 14451-14510
[15]
33 Taylor K E. Summarizing multiple aspects of model performance in a single diagram. J Geophys Res, 2001, 106: 7183-7192
[16]
34 Gao X, Shi Y, Song R, et al. Reduction of future monsoon precipitation over China: Comparison between a high resolution RCM simulation and the driving GCM. Meteorol Atmos Phys, 2008, 100: 73-86
[17]
35 Li Y F, Harrison S P. Simulations of the impact of orbital forcing and ocean on the Asian summer monsoon during the Holocene. Glob Planet Change, 2008, 60: 505-522
[18]
36 Marzin C, Braconnot P. The role of the ocean feedback on Asian and African monsoon variations at 6 kyr and 9.5 kyr BP. C R Geosci, 2009, 341: 643-655
[19]
39 Guiot J, Wu H B, Jiang W Y, et al. East Asian monsoon and paleoclimatic data analysis: A vegetation point of view. Clim Past, 2008, 4: 137-145
[20]
40 Jiang D, Lang X, Tian Z, et al. Last glacial maximum climate over China from PMIP simulations. Paleogeogr Paleoclimatol Paleoecol, 2011, 309: 347-357
[21]
41 Qin B, Yu G. Implications of lake level variations at 6 ka and 18 ka in mainland Asia. Glob Planet Change, 1998, 18: 59-72
[22]
42 Li Y, Morrill C. Lake levels in Asia at the last glacial maximum as indicators of hydrologic sensitivity to greenhouse gas concentrations. Quat Sci Rev, 2013, 60: 1-12
[23]
14 Long H, Lai Z P, Fuchs M, et al. Timing of Late Quaternary palaeolake evolution in Tengger Desert of northern China and its possible forcing mechanisms. Glob Planet Change, 2012, 92-93: 119-129
[24]
15 Bartlein P, Harrison S, Brewer S, et al. Pollen-based continental climate reconstructions at 6 and 21 ka: A global synthesis. Clim Dyn, 2011, 37: 775-802
[25]
16 Liu Z, Harrison S P, Kutzbach J, et al. Global monsoons in the mid-Holocene and oceanic feedback. Clim Dyn, 2004, 22: 157-182
[26]
17 Braconnot P, Otto-Bliesner B, Harrison S, et al. Results of PMIP2 coupled simulations of the mid-Holocene and last glacial maximum—Part 1: Experiments and large-scale features. Clim Past, 2007, 3: 261-277
[27]
18 Zhao Y, Harrison S P. Mid-Holocene monsoons: A multi-model analysis of the inter-hemispheric differences in the responses to orbital forcing and ocean feedbacks. Clim Dyn, 2012, 39: 1457-1487
[28]
19 Wang H J. Role of vegetation and soil in the Holocene megathermal climate over China. J Geophys Res, 1999, 104: 9361-9367
[29]
20 Chen X, Yu G, Liu J. The climatic simulations and discussion of temperature changes of mid-Holocene over East Asia (in Chinese). Sci China Ser D Earth Sci, 2002, 32: 335-345 [陈星, 于革, 刘健. 东亚中全新世的气候模拟及其温度变化机制探讨. 中国科学D辑: 地球科学, 2002, 32: 335-
[30]
21 Zhou B T, Zhao P. Inverse correlation between ancient winter and summer monsoons in East Asia? Chin Sci Bull, 2009, 54: 3760-3767 [周波涛, 赵平. 古东亚冬季风和夏季风反位相变化吗? 科学通报, 2009, 20: 3136-
[31]
23 Wang T, Wang H J, Jiang D. Mid-Holocene East Asian summer climate as simulated by the PMIP2 models. Paleogeogr Paleoclimatol Paleoecol, 2010, 288: 93-102
[32]
29 Adler R F, Huffman G J, Chang A, et al. The version 2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979-present). J Hydrometeorol, 2003, 4: 1147-1167
[33]
30 Berger A. Long-term variations of daily insolation and Quaternary climatic changes. J Atmos Sci, 1978, 35: 2362-2367
[34]
31 CLIMAP Project Members. Seasonal reconstructions of the Earth's surface at the last glacial maximum. Geol Soc Am Map Chart Ser MC-36, 1981
[35]
37 Jiang D, Tian Z, Lang X. Mid-Holocene net precipitation changes over China: Model-data comparison. Quat Sci Rev, 2013, 82: 104-120
[36]
38 Shi Y, Kong Z, Wang S, et al. Mid-Holocene climates and environments in China. Glob Planet Change, 1993, 7: 219-233
[37]
43 Yu G, Chen X, Ni J, et al. Palaeovegetation of China: A pollen data-based synthesis for the mid-Holocene and last glacial maximum. J Biogeogr, 2000, 27: 635-664
[38]
44 Ni J, Yu G, Harrison S P, et al. Palaeovegetation in China during the late Quaternary: Biome reconstructions based on a global scheme of plant functional types. Paleogeogr Paleoclimatol Paleoecol, 2010, 289: 44-61
[39]
45 Tang L Y, Shen C M, Liao G B, et al. Climatic changes in the southeastern Qinghai-Tibetan Plateau during the last glacial maximum—pollen records from southeastern Tibet (in Chinese). Sci China Ser D Earth Sci, 2004, 34: 436-442 [唐领余, 沈才明, 廖淦标, 等. 末次盛冰期以来西藏东南部的气候变化——西藏东南部的花粉记录. 中国科学D辑: 地球科学, 2004, 34: 436-
[40]
46 Wan H W, Tang L Y, Zhang H C, et al. Pollen record re?ects climate changes in eastern Qaidam Basin during 36-18 ka BP (in Chinese). Quat Sci, 2008, 28: 112-121 [万和文, 唐领余, 张虎才, 等. 柴达木盆地东部36~18 ka B.P.期间的孢粉记录及其气候环境. 第四纪研究, 2008, 28: 112-
[41]
47 Shi Y F, Zheng B X, Yao T D. Glaciers and environments during the last glacial maximum (LGM) on the Tibetan Plateau (in Chinese). J Glaciol Geocryol, 1997, 19: 97-113 [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: 97-
[42]
48 Xu Y, Gao X J, Giorgi F. Upgrades to the reliability ensemble averaging method for producing probabilistic climate-change projections. Clim Res, 2010, 41: 61-81
[43]
49 Gao X J, Zhao Z, Ding Y, et al. Climate change due to greenhouse effects in China as simulated by a regional climate model. Adv Atmos Sci, 2001, 18: 1224-1230
[44]
50 Gao X J, Shi Y, Giorgi F. A high resolution simulation of climate change over China. Sci China Earth Sci, 2011, 54: 462-472 [高学杰, 石英, Giorgi F. 中国区域气候变化的一个高分辨率数值模拟. 中国科学: 地球科学, 2010, 40: 911-
[45]
51 Ju L, Wang H J, Jiang D. Simulation of the Last Glacial Maximum climate over East Asia with a regional climate model nested in a general circulation model. Paleogeogr Paleoclimatol Paleoecol, 2007, 248: 376-390
[46]
1 Wang B, Ding Q H. Global monsoon: Dominant mode of annual variation in the tropics. Dyn Atmos Oceans, 2008, 44: 165-183
[47]
3 Liu J, Wang B, Ding Q H, et al. Centennial variations of the global monsoon precipitation in the last millennium: Results from ECHO-G Model. J Clim, 2009, 22: 2356-2371
[48]
4 Hsu P C, Li T, Luo J J, et al. Increase of global monsoon area and precipitation under global warming: A robust signal? Geophys Res Lett, 2012, 39: L06701, doi: 10.1029/2012GL051037
[49]
5 Wang B, Liu J, Kim H J, et al. Recent change of the global monsoon precipitation (1979-2008). Clim Dyn, 2012, 39: 1123-1135
[50]
8 Hsu P C, Li T, Murakami H, et al. Future change of the global monsoon revealed from 19 CMIP5 models. J Geophys Res, 2013, 118: 1247-1260
[51]
9 An C B, Feng Z D, Tang L Y. Evidence of a humid mid-Holocene in the western part of Chinese Loess Plateau. Chin Sci Bull, 2003, 48: 2472-2479 [安成邦, 冯兆东, 唐领余. 黄土高原西部全新世中期湿润气候的证据. 科学通报, 2003, 48: 2280-