Shen J, Liu X Q, Wang S M, et al. 2005. Palaeoclimatic changes in the Qinghai Lake area during the last 18000 years. Quat Int, 136: 131-140
[2]
Shi Y F, Shen Y P, Kang E, et al. 2007. Recent and future climate change in Northwest China. Clim Chang, 80: 379-393
[3]
Uno I, Eguchi K, Yumimoto K, et al. 2009. Asian dust transported one full circuit around the globe. Nat Geosci, 2: 557-560
[4]
Wang H, Wang B, Huang F, et al. 2012. Interdecadal change of the boreal summer circumglobal teleconnection (1958-2010). Geophys Res Lett, 39: L12704
[5]
Wang H J. 2001. The weakening of the Asian Monsoon circulation after the end of 1970''s. Adv Atmos Sci, 18: 376-386
[6]
Wang H J, Chen H P. 2012. Climate control for southeastern China moisture and precipitation: Indian or East Asian monsoon? J Geophys Res, 117: D12109
[7]
Wang W, Feng Z D. 2013. Spatial variations of effective moisture during the megathermal mid-Holocene in the East Asian arid and semiarid regions. Earth-Sci Rev, 122: 38-57
[8]
Wang Y, Cheng H, Edwards R L, et al. 2005. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science, 308: 854-857
[9]
Xiao J L, Xu Q H, Nakamura T, et al. 2004. Holocene vegetation variation in the Daihai Lake region of north-central China: A direct indication of the Asian monsoon climatic history. Quat Sci Rev, 23: 1669-1679
[10]
Yao T D, Thompson L, Yang W, et al. 2012. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nat Clim Chang, 2: 663-667
[11]
Zhou T J, Yu R C. 2005. Atmospheric water vapor transport associated with typical anomalous summer rainfall patterns in China. J Geophys Res, 110: D08104
Becker A, Finger P, Meyer-Christoffer A, et al. 2013. A description of the global land-surface precipitation data products of the Global Precipitation Climatology Centre with sample applications including centennial (trend) analysis from 1901-present. Earth Syst Sci Data, 5: 71-99
[23]
Chen F H, Yu Z C, Yang M L, et al. 2008. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quat Sci Rev, 27: 351-364
[24]
Chen F H, Chen J H, Holmes J, et al. 2010. Moisture changes over the last millennium in arid central Asia: A review, synthesis and comparison with monsoon region. Quat Sci Rev, 29: 1055-1068
[25]
Chen G S, Huang R H. 2012. Excitation mechanisms of the teleconnection patterns affecting the july precipitation in northwest china. J Clim, 25: 7834-7851
[26]
Chen J H, Chen F H, Feng S, et al. 2015. Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and little ice age: Spatial patterns and possible mechanisms. Quat Sci Rev, 107: 98-111
[27]
Chen M Y, Xie P P, Janowiak J E, et al. 2002. Global land precipitation: A 50-yr monthly analysis based on gauge observations. J Hydrometeorol, 3: 249-266
[28]
Ding Q H, Wang B. 2005. Circumglobal teleconnection in the Northern Hemisphere summer. J Clim, 18: 3483-3505
[29]
Ding Q H, Wang B, Wallace J M, et al. 2011. Tropical-extratropical teleconnections in boreal summer: Observed interannual variability. J Clim, 24: 1878-1896
[30]
Duchon C E. 1979. Lanczos filtering in one and two dimensions. J Appl Meteorol Clim, 18: 1016-1022
[31]
Enomoto T, Hoskins B J. Matsuda Y. 2003. The formation mechanism of the Bonin high in August. Q J R Meteorol Soc, 129: 157-178
[32]
Fang K Y, Davi N, Gou X H, et al. 2010. Spatial drought reconstructions for central High Asia based on tree rings. Clim Dyn, 35: 941-951
[33]
Feng S, Hu Q, Qian W H. 2004. Quality control of daily meteorological data in China 1951-2000: A new dataset. Int J Climatol, 24: 853-870
[34]
Feng S, Hu Q. 2008. How the North Atlantic Multidecadal Oscillation may have influenced the Indian summer monsoon during the past two millennia. Geophys Res Lett, 35: L01707
[35]
Feng S, Hu Q, Huang W, et al. 2014. Projected climate shift under future global warming from multi-model, multi-scenario, CMIP5 simulations. Glob Planet Change, 112: 41-52
[36]
Harris I, Jones P D, Osborn T J, et al. 2014. Updated high-resolution grids of monthly climatic observations-the CRU TS3.10 Dataset. Int J Climatol, 34: 623-642
[37]
Huang W, Chen F H, Feng S, et al. 2013. Interannual precipitation variations in the mid-latitude Asia and their association with large scale atmospheric circulation. Chin Sci Bull, 58: 3963-3968
[38]
Huang W, Feng S, Chen J H, et al. 2015. Physical mechanisms of the summer precipitation variations in the Tarim Basin, Northwestern China. J Clim, doi: 10.1175/JCLI-D-14-00395.1
[39]
Jin L Y, Chen F H, Morrill C, et al. 2012. Causes of early Holocene desertification in arid central Asia. Clim Dyn, 38: 1577-1591
[40]
Kalnay E, Kanamitsu M, Kistler R, et al. 1996. The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc, 77: 437-472
[41]
Liang E Y, Shao X M, Kong Z C, et al. 2003. The extreme drought in the 1920s and its effect on tree growth deduced from tree ring analysis: A case study in North China. Ann Forest Sci, 60: 145-152
[42]
Liu Z Y, Wen X Y, Brady E C, et al. 2014. Chinese cave records and the East Asia summer monsoon. Quat Sci Rev, 83: 115-128
[43]
Liu J P, Curry J A, Wang H J, et al. 2012. Impact of declining Arctic sea ice on winter snowfall. Proc Natl Acad Sci USA, 109: 4074-4079
[44]
Lorenz E N. 1956. Empirical orthogonal function and statistical weather prediction. Scientific Report No. 1 Statist Forecasting Project. Department of Meteorology, Massachusetts Institute of Technology
[45]
Lu R Y, Oh J H, Kim B J. 2002. A teleconnection pattern in upper-level meridional wind over the North African and Eurasian continent in summer. Tellus, 54A: 44-55
