8 Zhou J S, Yu Y Q, Liu H L, et al. Progress in the development and application of Climate Ocean Models and Ocean-atmosphere CoupledModels in China. Adv Atmos Sci, 2007, 24: 1109-1120？？
19 Zhou T J, Wu B, Wen X Y, et al. A fast version of LASG/IAP climate system model and its 1000-year control integration. Adv Atmos Sci,2008, 25: 655-672？？
[10]
20 Wen X Y, Zhou T J, Wang S W, et al. Performance of a Reconfigured Atmospheric General Circulation Model at low resolution. AdvAtmos Sci, 2007, 24: 712-728
[11]
21 Crowley T J. Causes of climate changes over the past 1000 years. Science, 2000, 289: 270-277？？
[12]
22 Xie P P, Arkin P A. Global precipitation: A 17-year monthly analysis based on gauge observations, satellite estimates, and numericalmodel outputs. Bull Amer Meteor Soc, 1997, 78: 2539-2558？？
28 Yu R C, Li W, Zhang X H, et al. Climatic features related to eastern China summer rainfalls in the NCAR CCM3. Adv Atmos Sci, 2000,17: 503-518？？
[15]
29 Chen H M, Zhou T J, Neale R B, et al. Performance of the new NCAR CAM3.5 in East Asian Summer Monsoon simulation: Sensitivity tomodifications of the Convection Scheme. J Clim, 2010, 23: 3657-3675
[16]
30 Zhou T J, Li Z X. Simulation of the east Asian summer monsoon by using a variable resolution atmospheric GCM. Clim Dyn, 2002, 19:167-180？？
[17]
31 Zou L W, Zhou T J, Li Z X, et al. East China summer rainfall variability of 1958-2000: Dynamical downscaling with a variable-resolutionAGCM. J Clim, 2010, 23: 6394-6408？？
[18]
32 Li L J, Wang Y Q, Wang B, et al. Sensitivity of the Grid-point Atmospheric Model of IAP LASG (GAMIL1.1.0) climate simulations tocloud droplet effective radius and liquid water path. Adv Atmos Sci, 2008, 25: 529-540
[19]
33 Zhou T J, Yu R C. Atmospheric water vapor transport associated with typical anomalous summer rainfall patterns in China. J GeophysRes, 2005, 110: D08104
[20]
36 Chang C P, Zhang Y S, Li T. Interannual and interdecadal variation of the East Asian summer monsoon and tropical Pacific SSTs. J Clim,2000, 13: 4310-4340？？
39 Wang B, Zhang Q. Pacific-East Asian teleconnection. Part II: How the Philippine Sea anomalous anticyclone is established during El Ni？odevelopment. J Clim, 2002, 15: 3252-3265
[23]
42 Widmann M, Tett S F B. Simulating the climate of the last millennium. IGBP Newslett, 2004, 56: 10-13
[24]
43 Shindell D T, Schmidt G A, Mann M E, et al. Solar forcing of regional climate change during the Maunder Minimum. Science, 2001, 294:2149-2152？？
[25]
44 Ammann C M, Joos F, Schimel D S, et al. Solar influence on climate during the past millennium: Results from transient simulations withthe NCAR Climate System Model. Proc Natl Acad Sci USA, 2007, 104: 3713-3718？？
9 Zhou T J, Yu R C. Twentieth century surface air temperature over China and the globe simulated by coupled climate models. J Clim, 2006,19: 5843-5858？？
18 Yu Y Q, Zhi H, Wang B, et al. Coupled model simulations of climate changes in the 20th century and beyond. Adv Atmos Sci, 2008, 25:641-654？？
[36]
23 Dai A G, Wigley T M L, Boville B A, et al. Climates of the 20th and 21st centuries simulated by the NCAR Climate System Model. JClim, 2001, 14: 485-519
[37]
24 Manabe S, Wetherald R T. Thermal equilibrium of the atmosphere with a given distribution of relative humidity. J Atmos Sci, 1967, 24:241-259？？
34 Liu J, Wang B, Wang H L, et al. Forced response of the East Asian summer rainfall over the past millennium: Results from a coupledmodel simulation. Clim Dyn, 2010, doi: 10.1007/s00382-009-0693-6
[41]
35 Shen S, Lau K M. Biennial oscillation associated with the East Asian summer monsoon and tropical Pacific sea surface temperatureanomalies. J Meteor Soc Jpn, 1995, 73: 105-124
[42]
38 Wang B, Wu R G, Fu X H. Pacific-East Asian teleconnection: How does ENSO affect East Asian climate? J Clim, 2000, 13: 1517-1536
[43]
40 Wu B, Zhou T J, Li T. Seasonally evolving dominant interannual variability modes of East Asian Climate. J Clim, 2009, 22: 2992-3005？？
