[1] BEI N, ZHANG F. Impacts of initial errorscale andamplitude on the mesoscale predictability of heavyprecipitation along the mei-yu front of China [J]. Quart. J. Roy.Meteor. Soc., 2007, 133: 83-99.
[2] WANG Xiao-fang, XU Ming, MIN Ai-rong, et al. Analysisof precipitation and affecting systems features on persistentheavy rain in South China in May 2010 [J]. Torrent. RainDisast., 2010, 29: 193-199.
[3] ZHANG Qing-yun, TAO Shi-yan, ZHANG Shun-li. Thepersistent heavy rainfall over the Yangtze River Valley and itsassociations with the circulations over East Asian duringsummer [J]. Chin. J. Atmos. Sci., 2003, 27: 1018-1030.
[4] WANG Zun-ya, DING Yi-hui. Climatic characteristics ofrainy seasons in China [J]. Chin. J. Atmos. Sci., 2008, 32: 1-11.
[5] YANG Qiu-ming. The 20-30-day oscillation of the globalcirculation and heavy precipitation over the lower reaches ofthe Yangtze River valley [J]. Sci. China (Ser. D: Earth Sci.),2009, 52: 1485-1501, doi: 10.1007/s11430-009-0156-2.
[6] LI Chong-yin. The Low-Frequency Oscillation of theAtmosphere [M]. Beijing: China Meteorological Press, 1993:50-56.
[7] MURAKAMI T, NAKAZAWA T, HE J H. On the 40-50day oscillation during the 1979 Northern Hemisphere summer,Part I: Phase propagation [J]. J. Meteor. Soc., Japan, 1984, 62:440-468.
[8] CHEN Long-xun, LUO Shao-hua, SHEN Ru-gui. Thestructure of the Asian Summer Monsoon circulation and itsrelationship with the seasonal variation of the generalcirculation [C]// The Collected Works of the Tropical SynopticConference in 1980. Beijing: Science Press, 1982: 82-99.
[9] JU Jian-hua, QIAN Chen, CAO Jie. The intraseasonaloscillation of East Asian summer monsoon [J]. Chin. J. Atmos.Sci., 2005, 29: 187-194.
[10] ZHU Qian-gen, YANG Song. The northward advance andoscillation of the East Asian Summer Monsoon [J]. J. NanjingInst. Meteor., 1989, 12: 249-257.
[11] HAN Rong-qing, LI Wei-jing, DONG Min. A diagnosticstudy of the temporal and spatial characteristics of theintraseasonal oscillation over the subtropical northern Pacific[J]. Acta Meteor. Sinica, 2010, 68: 520-528.
[12] WALISER D E, STERN W, SCHUBERT S, et al.Dynamical predictability of intraseasonal variability associated with the Asian summer monsoon [J]. Quart. J. Roy. Meteor.Soc., 2003, 129: 2897-2925.
[13] SWINBANK R, PALMER T N, DAVEY M K. Numericalsimulations of the Madden and Julian oscillation [J]. J. Atmos.Sci., 1988, 45: 774-788.
[14] FERRANTI L, PALMER T N, MOLTENI F, et al.Tropical-extratropical interaction associated with the 30-60days oscillation and its impact on medium and extended rangeprediction [J]. J. Atmos. Sci, 1990, 47: 2177-2199.
[15] MATTHEWS A J, LI H Y Y. Modulation of station rainfallover the western Pacific by the Madden-Julian oscillation [J].Geophys. Res. Lett., 2005, 32: L14827, doi: 10.1029/2005GL023595.
[16] GOSWAMI B N, XAVIER P K. Potential predictabilityand extended range prediction of Indian summer monsoonbreaks [J]. Geophys. Res. Lett., 2003, 30(18): 1966,doi: 10.1029/2003GL017810.
[17] DING Q H, WANG B. Intraseasonal teleconnectionbetween the summer Eurasian wave and the Indian monsoon[J]. J. Climate, 2007, 20: 3751-3767.
[18] GOSWAMI B N, WU G X, YASUNARI T. The annualcycle, intraseasonal oscillations, and roadblock to seasonalpredictability of the Asian summer monsoon [J]. J. Climate,2006, 19: 5078-5099.
[19] HAN Rong-qing, LI Wei-jing, DONG Min. The impact of30-60 day oscillations over the subtropical Pacific on the EastAsian summer rainfall [J]. Acta Meteor. Sinica, 2006, 64:149-163.