[1] QIAN W H, LIN X, ZHU Y F, et al. Climatic regime shiftand decadal anomalous events in China [J]. Climatic Change,2007, DOI 10.1007/s10584- 006-9234-z.
[2] QIAN Wei-hong, ZHU Jiang, WANG Yong-guang, et al.Regional relationship between the Jiang-Huai Meiyu and theequatorial surface-subsurface temperature anomalies [J]. Chin.Sci. Bull., 2008, 10.1007/s11434-008-0410-6.
[3] WU Shang-sen, Liang Jian-yin. Temporal and Spatialcharacteristics of the drought and flood during the rainyseason in South China [J]. J. Trop. Meteor., 1992, 8(1): 87-92.
[4] LIN Ai-lan, WU Shang-sen. Variations and trend predictionof rainfall of rainy season in South China in 1951-1991[J]. J.Trop. Meteor., 1996, 12(2): 160-166.
[5] DENG Li-ping, WANG Qian-qian. On the relationshipbetween precipitation anomalies in the first raining season(April-June) in southern China and SST over offshore waters inChina [J]. J. Trop. Meteor., 2002, 18(1): 45-55.
[6] LIANG Jian-yin. The interannual variations of the subtropichigh ridge position over western pacific in June and itsinfluence on precipitation in South of China [J]. J. Trop.Meteor., 1994, 10(3): 274-279.
[7] LIANG Jian-yin, WU Shang-sen. Formation reasons ofdrought and flood in the rain season of Guangdong andpreceding impact factors [J]. J. Trop. Meteor., 2001, 17(2):97-108.
[8] TAO Shi-yan, WEI Jie, ZHANG Xiao-ling. Large-scaleFeatures of the Mei-Yu Front Associated with Heavy Rainfallin 2007 [J]. Meteor. Mon., 2008, 34(4): 3-15.
[9] SHI Xue-li, DING Yi-hui. A study on extensive heavy rainprocesses in South China and the summer monsoon activity in1994 [J]. Acta Meteor. Sinica, 2000, 58(6): 666-677.
[10] LIN Ai-lan, LIANG Jian-yin, LI Chun-hui, et al. Monsooncirculation background of ‘0506’ continuous rainstorm in SouthChina [J]. Adv. Water Sci., 2007, 18(3): 424-432.
[11] XIE Jiong-guang, JI Zhong-ping. The relation between seasurface temperature of the North-West Pacific Ocean andfloods season rainfall of Guangdong Provinc [J]. J. Trop.Meteor., 1999, 15(1): 56-63.
[12] GOSWAMI B N, VENUGOPAL V, SENGUPTA D, et al.Increasing trend of extreme rain events over India in a warmingenvironment [J]. Sci., 2006, 314: 1 442-1 445.
[13] YAO C, YANG S, QIAN W H, et al. Regional summerprecipitation events in Asia and their changes in the pastdecades [J]. J. Geophys. Res., 2008, 113, D17107,doi: 10.1029/2007JD009603.
[14] ZHOU Lian-tong, HUANG Rong-hui. Research on thecharacteristics of interdecadal variability of summer climate inChina and Its possible cause [J]. Clim. Environ. Res., 2003,8(3): 274-290.
[15] LI Chun-hui, LIANG Jian-yin. A preview of activities ofsummer monsoon over South China Sea in 2004 [J]. J. Trop.Meteor., 2005, 21(6): 561-569.
[16] MA Hui, CHEN Zhen-hua. Climate background of heavyrains in June 2005 in south China [J]. J. Guangdong Meteor.,2005(4): 14-16.
[17] XIE P A, YATAGAI M Y, CHEN T, et al. A gauge-basedanalysis of daily precipitation over East Asia [J]. JHydrometeor. 2007, 8(3): 607-626.
[18] KISTLER R, COLLINS W, SAHA S, et al. TheNCEP-NCAR 50-year reanalysis: monthly means CD-ROMand documentation[J]. Bull. Am. Meteor. Soc., 2001, 82(2):247-268.
[19] SMITH T M, REYNOLDS R W, PETERSON T C, et al.Improvements to NOAA's historical merged land-ocean surfacetemperature analysis (1880-2006) [J]. J. Climate, 2008, 21(1):2283-2296.
[20] MA Hui, WANG Qian-qian, CHEN Zhen-hua. Spatial andtemporal variations in pre-summer flood period precipitation ofsouth China [J]. Plateau Meteor., 2006, 25(2): 325-329.
[21] QIAN W H, QIN A M. Precipitation division and climateshift in China from 1960 to 2000 [J]. Theor. Appl. Climatol.,2008, doi: 10.1007/s00704-007-0330-4.
[22] DING Zhi-ying, CHANG Yue, ZHU Li, et al. Research onthe reason of the double rain -bands’ forming in a sustainingstorm rainfall of South China [J]. J. Trop. Meteor., 2008, 24(2):117-124.
[23] ASHOK K, BEHERA S K, RAO S A, et al. El NiñoModoki and its possible teleconnection [J]. J. Geophys.Res.-Ocean, 2007, 112(11): C11007.