Rayner N A,Horton E B,Parker D E,et al.Version 2.2 of the Global sea-Ice and SeaSurface Temperature Data Set,1903-1994.Climate Research Technical Note 74,unpublisheddocument available from Hadley Centre for Climate Prediction and Research.MeteorologicalOffice,London Road,Bracknell,RS12 2SY,U.K.,1996
[3]
Plumb R A.On the three-dimensional propagation of stationarywaves.J.Atmos.Sci.,1985,42:217～229
[4]
Lau K M,Kim K M,Yang S.Dynamical and boundary forcing characteristics of regionalcomponents of the Asian summer monsoon.J.Climate,2000,13:2461～2481
[5]
Chen L X,Dong M,Shao Y N.The characteristics of interannual variations of the EastAsian monsoon.J.Meteor.Soc.Japan,1992,70:397～421
[6]
Krishnan R,Sugi M.Baiu rainfall variability and associated monsoonteleconnections.J.Meteor.Soc.Japan,2001,79 (3):851～860
[7]
Enomoto T,Hoskins B J,Matsuda Y.The formation mechanism of the Bonin high inAugust.J.Meteor.Soc.Japan,2003,129:157～178
[8]
Ambrizzi T,Hoskins B J,Hsu H H.Rossby wave propagation and teleconnection patterns inthe Austral winter.J.Atmos.Sci.,1995,52:3661～3672
[9]
孙安健.江淮流域旱涝年份准定常行星波分布与平均纬向风速的差异.应用气象学报,1994,5(1):68～76 Sun Anjian.The differences of quasi-stationary planetary wave distribution andmean zonal wind speed between drought and flood years in summer in the Changjiang andHuaihe River basins.Quart.J.Appl.Meteor.(in Chinese),1994,5(1):68～76
[10]
Liang X Z,Wang W C.Association between China monsoon rainfall and troposphericjets.Quart.J.Roy.Meteor.Soc.,1998,124:2597～2623
[11]
Lu R Y,Oh J H,Kim B J.A teleconnection pattern in upper-level meridional wind over theNorth African and Eurasian continent in summer.Tellus,2002,54A:44～55
[12]
Park C K,Schubert S D.On the nature ofthe 1994 East Asian summer drought.J.Climate,1997,10:1056～1070
[13]
Trenberth K E,Guillemot C J.Physical processes involved in the 1988 drought and 1993floods in North America.J.Climate,1996,9:12881～1298
[14]
Yoo S H,Ho C H,Yang S.Influences of tropical western and extratropical Pacific SST onEast and Southeast Asian climate in the summers of 1993-1994.J.Climate,2004,17:2673～2687
[15]
Huang R H.The characteristics of the forced planetary wave propagations in the summerNorthern Hemisphere.Adv.Atmos.Sci.,1984,1:85～94
[16]
Huang R H.Numerical simulation of the three-dimensional teleconnections in the summercirculation over the Northern Hemisphere.Adv.Atmos.Sci..1985,2:81～92
[17]
Nitta T.Convective activities in the tropical Western Pacific and their impact on theNorthern Hemisphere summer circulation.J.Meteor.Soc.Japan,1987,65:373～390
[18]
闵锦忠,李春,吴凡.夏季热带西太平洋对流与长江中下游降水关系的研究.大气科学,2005,29(6):947～954 Min Jinzhong,Li Chun,Wu Fan.A study of the relationship between summertropical convection over the Western Pacific and the rainfall in the middle-lower reachesof the Yangtze River.Chinese Journal of Atmospheric Sciences (in Chinese),2005,29 (6):947～954
[19]
Xie P,Arkin P A.Global precipitation:A 17-year monthly analysis based on gaugeobservations,satellite estimates and numerical modeloutputs.Bull.Amer.Meteor.Soc.,1997,78:2539～2558
[20]
Enomoto T.Interannual variability of the Bonin high associated with the propagation ofRossby waves along the Asian Jet.J.Meteor.Soc.Japan,2004,82 (4):1019～1033
[21]
黄荣辉,孙凤英.热带西太平洋暖池的热状态及其上空的对流活动对东亚夏季气候异常的影响.大气科学,1994,18(2):141～151 Huang Ronghui,Sun Fengyin.Impacts of the thermal state and the convectiveactivities in the tropical Western Warm pool on the summer climate anomalies in EastAsia.Chinese Journal of Atmospheric Sciences (Scientia Atmospheric Sinica) (inChinese),1994,18 (2):141～151
[22]
Nitta T.Convective activities in the tropical western Pacific and their impact on theNorthern Hemisphere summer circulation.J.Meteor.Soc.Japan,1987,65:373～390
