[1] ZENG Qing-cun, LI Jian-ping. Interaction between thenorthern and southern hemispheric atmospheres and theessence of monsoon [J]. Chin. J. Atmos. Sci., 2002, 26:433-448.
[2] YASUNARI T. Impact of Indian monsoon on the coupledatmosphere/ocean system in the tropical Pacific [J]. Meteor. & Atmos. Phys., 1990, 44: 29-41.
[3] WEBSTER P J, YANG S. Monsoon and ENSO: selectiveinteraction system [J]. Quart. J. R. Meteor. Soc., 1992, 118:877-926.
[4] WU Guo-xiong, MENG Wen. Gear between theIndo-monsoon circulation and the Pacific-Walker circulationand ENSO. PartⅠ: Data analyses [J]. Chin. J. Atmos. Sci.,1998, 22: 470-480.
[5] LAU K M, WU H T. Principal Modes of rainfall-SSTvariability of the Asian summer monsoon: A reassessment ofthe monsoon-ENSO relationship [J]. J. Climate, 2001, 14:2880-2895.
[6] LI Chong-yin, CHEN Yu-xing, YUAN Chong-guang. Animportant reason for the occurrence of El Ni?oevents―frequency activity of east winter monsoon [J]. Chin. J.Atmos. Sci., 1988, 12(special issue): 125-132.
[7] LI Chong-yin, MU Ming-quan. Numerical simulation ofanomalous winter monsoon in East Asian exciting ENSO [J].Chin. J. Atmos. Sci., 1998, 22: 481-490.
[8] WANG Qi, LIU Qin-yu, HU Rui-jin, et al. A possible roleof the South China Sea in ENSO cycle [J]. Acta Oceanol.Sinica, 2002, 21 (2): 217-226.
[9] YAN Jin-yue. Climatological characteristics on the onset ofthe South China Sea southwest monsoon [J]. Acta Meteor.Sinica, 1997, 55(2): 174-186.
[10] LIU Xia, XIE An, YE Qian, et al. The climaticcharacteristics of summer monsoon onset over South ChinaSea [J]. J. Trop. Meteor., 1998, 14: 28-37.
[11] LI Chong-yin, ZHANG Li-ping. Summer monsoonactivities in the South China Sea and its impacts [J]. Chin. J.Atmos. Sci., 1999, 23: 257-266.
[12] KALNAY E, et al. The NCEP/NCAR 40 year reanalysisproject [J]. Bull. Amer. Meteor. Soc., 1996, 77: 437-471.
[13] SMITH T M, REYNOLDS R W. Improved ExtendedReconstruction of SST (1854-1997) [J]. J. Climate, 2004, 17:2466-2477.
[14] XIE P, ARKIN P A. Analyses of Global MonthlyPrecipitation Using Gauge Observations, Satellite Estimatesand Numerical Model Predictions [J]. J. Climate, 1996, 9:840-858.
[15] XIE P, ARKIN P A. Global Precipitation: A 17-yearmonthly analysis based on gauge observations, satelliteestimates and numerical model outputs [J]. Bull. Amer. Meteor.Soc., 1997, 78: 2539-2558.
[16] WU Shang-sheng, LIANG Jian-yin. An index of SouthChina Sea summer monsoon intensity and its variationcharacteristics [J]. J. Trop. Meteor., 2001, 17: 337-334.
[17] YANG S, K M LAU, KIM K M. Variations of the EastAsian jet stream and Asian-Pacific-American winter climateanomalies [J]. J. Climate, 2002, 15: 306-325.
[18] XUE Feng, WANG Hui-jun, HE Jin-hai. Interannualvariability of Mascarene high and Australian high and theirinfluence on summer rainfall over East Asia [J]. Chin. Sci.Bull., 2003, 48: 492-497.
[19] LIANG Jian-yin, WU Shang-sheng. The multi-time scalevariations of summer monsoon over South China Sea and itsinteraction with SST anomaly [J]. Quart. J. Appl. Meteor.,2000, 11: 95-104.
[20] CHANG C P, ZHANG Y S, LI T. Interannual andinterdecadal variations of the East Asian summer monsoon andtropical Pacific SSTs. Part I: Role of subtropical ridges [J]. J.Climate, 2000, 13: 4310-4325.
[21] WANG B, WU R, FU X. Pacific-East Asia teleconnection:How does ENSO affect East Asian climate? [J]. J. Climate,2000, 13: 1517-1536.
[22] HONG C C, LI T, LINHO J S, et al. Asymmetry of theIndian Ocean Dipole. Part I: Observational analysis [J]. J.Climate, 2008, 21: 4834-4848.
[23] HONG C C, LI T, LUO J J. Asymmetry of the IndianOcean Dipole. Part II: Model diagnosis [J]. J. Climate, 2008,21: 4849-4858.
[24] WU Guo-xiong, CHOU Ji-fan, LIU Yi-min, et al.Dynamics of the Formation and Variation of Subtropical High[M]. Beijing: Science Press, 2002: 79-84.
[25] MIAO Quan-sun, ZHAO Zhen-guo. The RelationshipBetween Blocking Situation of East Asia and Subtropical Highof Western Pacific and Its Impact on China Rainfall [M].Collection of papers on long-tern weather forecast. Beijing:Meteorology Press, 1990: 125-134.
[26] HUANG Rong-hui, LI Wei-jing. The impact of summerthermal anomalies over tropical west Pacific on subtropicalhigh over East Asia and its physical mechanism [J]. Chin. J.Atmos. Sci., 1988, 12(special issue): 107-116.
[27] WALLACE J M, GUTZLER D S. Teleconnections in thegeopotential height field during the Northern Hemispherewinter [J]. Mon. Wea. Rev., 1981: 109, 784-812.
[28] GILL A E. Some simple solutions for heat-inducedtropical circulation [J]. Quart. J. Roy. Meteor. Soc., 1980, 106:447-462.
[29] WEBSTER P J, MOORE A, LOSCHNIGG J, et al.Coupled ocean-atmosphere dynamics in the Indian Oceanduring 1997-98 [J]. Nature, 1999, 401: 356-360.
[30] LI T, WANG B, CHANG C P, et al. A theory for theIndian Ocean dipole-zonal mode [J]. J. Atmos. Sci., 2003, 60:2119-2135.
[31] WANG B, WU R, LI T. Atmosphere-warm ocean interaction and its impact on Asian-Australian monsoonvariation [J]. J. Climate, 2003, 16: 1195-1211.
[32] KAJIKAWA Y, YASUNARI T, KAWAMURA R. The Roleof the local Hadley circulation over the western Pacific on thezonally asymmetric anomalies over the Indian Ocean [J]. J.Meteor. Soc. Japan, 2003, 81: 259-276.
[33] LI T, ZHANG Y, LU E, et al. Relative role of dynamicand thermodynamic processes in the development of the IndianOcean dipole: An OGCM diagnosis [J]. Geophys. Res. Lett.,2002, 29 (23), 2110, doi: 10.1029/2002GL05789.
[34] LI T, LIU P, FU X et al. Tempo-spatial structures andmechanisms of the tropospheric biennial oscillation in theIndo-Pacific warm ocean regions [J]. J. Climate, 2006, 19:3070-3087.
[35] MEEHL G A. The annual cycle and interannualvariability in the tropical Indian and Pacific Ocean regions [J].Mon. Wea. Rev., 1987, 115: 27-50.
[36] PHILANDER S G H, YAMAGATA T, PACANOWSKI RC. Unstable air-sea interaction in the tropics [J]. J. Atmos. Sci.,1984, 41: 604-613.
[37] WYRTKI K. El Ni?o－the dynamic response of theequatorial Pacific Ocean to atmospheric forcing [J]. J. Phys.Oceanogr., 1975, 5: 572-584.
[38] RASMUSSON E M, CARPENTER T H. Variations intropical sea surface temperature and surface wind fieldsassociated with the Southern Oscillation/El Ni?o [J]. Mon.Wea. Rev., 1982, 110: 354-384.
[39] DING Yi-hui. Analysis of large scale flow pattern duringTOGA COARE IOP [J]. Acta Meteor. Sinica, 1998, 56:284-295.