[1] MADDEN R A, JULIAN P R. Detection of a 40-50 dayoscillation in the zonal wind in the tropical Pacific [J]. J.Atmos. Sci., 1971, 28: 702-708.
[2] MADDEN R A, JULIAN P R. Description of global scalecirculation cells in the tropics with 40-50 day period [J]. J.Atmos. Sci., 1972, 29: 1109-1123.
[3] JONES C, WALISER D E, SCHEMM J K, et al.Predication skill of the Madden-Julian Oscillation indynamical extended range forecasts [J]. Climate Dyn., 2000,16: 273-289.
[4] LI C Y, JIA X L, DONG M. Numerical simulation andcomparison study of the atmospheric intraseasonal oscillation.[J]. Acta Meteor. Sinica, 2007, 21(1): 1-8.
[5] SLINGO J M, SPERBER K R, BOYLE J S, et al.Intraseasonal oscillation in 15 atmospheric general circulationmodels: Results from an AMIP diagnostic subproject [J].Climate Dyn., 1996, 12: 325-357.
[6] SPERBER K R. Madden-Julian variability in NCAR CAM2.0 and CCSM2.0 [J]. Climate Dyn., 2004, 23: 259-278.
[7] DUFFY P B, GOVINDASAMY B, IORIO J P, et al.High-resolution simulations of global climate I: Presentclimate [J]. Climate Dyn., 2003, 21: 371-390.
[8] INNESS P M, INNESS P M, WOOLNOUGH S J, et al.Organization of tropical convection in a GCM with varyingvertical resolution; implications for the simulation of theMadden-Julian Oscillation [J]. Climate Dyn., 2001, 17:777-793.
[9] JIA Xiao-long, LI Chong-yin, LING Jian, et al. Impacts ofthe GCM’s Resolution on the MJO Simulation [J]. Adv. Atmos.Sci., 2008, 25(1): 139-156.
[10] WANG W, SCHLESINGER M E. The dependence onconvection Parameterization of the tropical intraseasonaloscillation simulated in the UIUC 11-layer atmospheric GCM[J]. J. Climate, 1999, 12(5): 1423-1457.
[11] MALONEY E D, HARTMANN D L. The sensitive ofintraseasonal variability in the NCAR CCM3 to changes inconvection parameterization [J]. J. Climate, 2001, 14(9):2015-2034.
[12] RAJENDRAN K, RAVI S, NANJUNDIAH, et al.Comparison of seasonal and intraseasonal variation of tropicalclimate in NCAR CCM2 GCM with two different cumulusschemes [J]. Meteor. Atmos. Phys., 2002, 79(1): 57-86.
[13] LIU P, WANG B, SPERBER K R, et al. MJO in theNCAR CAM2 with the Tiedtke convection scheme [J]. J.Climate, 2005, 18(15): 3007-3020.
[14] EDWARDS J M, SLINGO A. Studies with a flexible newradiation code I：Choosing a configuration for a large-scalemodel [J]. Quart. J. Roy. Meteor. Soc., 1996, 122: 689-719.
[15] SLINGO J M. A cloud parameterization scheme derivedfrom GATE data for use with a numerical model [J]. Quart. J.R. Meteor. Soc., 1980, 106: 747-770.
[16] SLINGO J M. The development and verification of acloud prediction scheme for the ECMWF model [J]. Quart. J.Roy. Meteor. Soc., 1987, 113: 899-927.
[17] HOLTSLAG A A M, BOVILLE B. Local versus nonlocalboundary-layer diffusion in a global climate model [J]. J.Climate, 1993, 6(10): 1825-1842.
[18] XUE Y, SELLERS P J, LINTER J L, et al. A simplifiedbiosphere model for global climate studies [J]. J. Climate,1991, 4(3): 345-364.
[19] WANG Zai-zhi, WU Guo-xiong, LIU Ping, et al. Thedevelopment of GOALS/LASG AGCM and its globalclimatological features in climate simulation I: Influence ofhorizontal resolution [J]. J. Trop. Meteor., 2005, 21(3):225-237.
[20] WANG Zai-zhi, YU Ru-cong, WANG Peng-fei, et al. Thedevelopment of GOALS/LASG AGCM and its globalclimatological features in climate simulation II: the increase ofvertical resolution and its influence[J]. J. Trop. Meteor., 2005,21(3): 238-247.
[21] MANABE S, SMAGORINSKY J, STRICKLER R F.Simulated climatology of general circulation model with ahydrologic cycle [J]. Mon. Wea. Rev., 1965, 93(12): 769-798.
[22] ZHANG G J, MCFARLANE N A. Sensitivity of climatesimulation to the parameterization of cumulus convection inthe Canadian Climate Centre General Circulation Model [J].Atmos.-Ocean, 1995, 33: 407-446.
[23] TIEDTKE M. A comprehensive mass flux scheme forcumulus parameterization in large-scale models [J]. Mon. Wea.Rev., 1989, 117(8): 1779-1800.
[24] KALNAY E, COAUTHORS. The NCEP/NCAR 40-YearReanalysis Project [J]. Bull. Am. Meteor. Soc., 1996, 77(3):437-471.
[25] XIE P, ARKIN P A. Global precipitation: A 17-yearmonthly analysis based on gauge observations, satelliteestimates, and numerical model output [J]. Bull. Am. Meteor.Soc., 1997, 78(11): 2539-2558.
[26] MALONEY E D, HARTMANN D L. Frictional moistureconvergence in a composite life cycle of the Madden-Julianoscillation [J]. J Climate, 1998, 11(9): 2387-2403.
[27] Li Chong-yin. Convection condensation heating andunstable modes in the atmosphere [J]. Chin. J. Atmos. Sci.,1983, 7(3): 260-268.
[28] LI Chong-yin, JIA Xiao-long, LING Ji-an, et al.Sensitivity of MJO Simulations to Convective Heating Profiles[J]. Climate Dyn., 2009, 32(2):167-187.