Ding Y H.Synoptic processes in monsoons.The Global Monsoon System:Research and Forecast,WMO/TD NO.1266,2005,492～511
[2]
Koteswaram P.The easterly jet stream in the tropics.Tellus,1958,10:43～57
[3]
Kanamitsu M,Krishnamurti T N.Northern summer tropical circulations during drought and normal rainfall months.Mon.Wea.Rev.,1978,106:331～347
[4]
Tanaka M.Interannual fluctuations of the tropical easterly jet and the summer monsoon in the Asian region.J.Meteor.Soc.Japan,1982,60:865～875
[5]
Arkin P A.The relationship between interannual variability in the 200mb tropical wind field and Southern Oscillation.Mon.Wea.Rev.,1982,110:1393～1404
[6]
曾昭美,郭其蕴.亚非季风区夏季降水与热带东风急流的关系.大气科学,1982,6:283～292 Zeng Zhaomei,Guo Qiyun.The relationship between the summer precipitation over Asia-Africa monsoon regions and the tropical easterly jetstream.Chinese Journal of Atmospheric Sciences (Scientia Atmospherica Sinica) (in Chinese),1982,6:283～292
Simmons A J,Gibson J K,Eds.The ERA-40 Project Plan.ERA-40 Project Report Series 1,ECMWF,2000.62pp
[9]
陈桦,丁一汇,何金海.亚洲夏季风指数的重新评估与季风的长期变化.气象学报,2006,6:770～778 Chen Hua,Ding Yihui,He Jinhai.Reappraisal of the Asian summer monsoon indices and the long-term variation of monsoon.Acta Meteorologica Sinica (in Chinese),2006,6:770～778
[10]
Xie P P,Arkin P A.Analyses of global monthly precipitation using gauge observations,satellite estimates,and numerical model predictions.J.Climate,1996,9:840～858
[11]
Lu J X,Ding Y H.Climatic study on the summer tropical easterly jet at 200 hPa.Adv.Atmos.Sci.,1989,6:215～226
[12]
Webster P J,Yang S.Monsoon and ENSO:Selectively interactive systems.Quart.J.Roy.Meteor.Soc.,1992,118:877～926
[13]
Chase T N,Knaff J A,Pielke Sr.R A,et al.Changes in global monsoon circulations since 1950.Natural Hazards,2003,29:229～254
[14]
Trenberth K E,Hurrel J W.Decadal atmosphere-ocean variations in the Pacific.Climate Dyn.,1994,9:303～319
[15]
Wang H J.The weakening of the Asian monsoon circulation after the end of 1970\'s.Adv.Atmos.Sci.,2001,18:376～386
[16]
Nicholson S E,Grist J P.The seasonal evolution of the atmospheric circulation over West Africa and equatorial Africa.J.Climate,2003,16:1013～1030
[17]
Annamalai H,Slingo J M,Sperber K R,et al.The mean evolution and variability of the Asian summer monsoon:Comparison of ECMWF and NCEP-NCAR reanalyses.Mon.Wea.Rev.,1999,127:1157～1186
[18]
Newman M,Sardeshmukh P D,Bergman J W.An assessment of the NCEP,NASA,and ECMWF reanalyses over the tropical west Pacific warm pool.Bull.Amer.Meteor.Soc.,2000,81:41～48
[19]
Sturaro G.A closer look at the climatological discontinuities present in the NCEP/NCAR reanalysis temperature due to the introduction of satellite data.Climate Dyn.,2003,21:309～316
[20]
李新周,马柱国,刘晓东.中国北方干旱化年代际特征与大气环流的关系.大气科学,2006,2:277～284 Li Xinzhou,Ma Zhuguo,Liu Xiaodong.Inter-decadal characteristics of aridification over northern China associated with the variation of atmospheric circulation during the past 50 years.Chinese Journal of Atmospheric Sciences (in Chinese),2006,2:277～284
[21]
Palmén E.On the formation and structure of tropical cyclones.Geophysica,1948,3:26～38
[22]
陈联寿,丁一汇.西太平洋台风概论.北京:科学出版社,1979.1～10 Chen Lianshou,Ding Yihui.Introduction of the Western Pacific Typhoon (in Chinese).Beijing:Science Press,1979.1～10
[23]
Cressman G P.Circulations of the West Pacific jet stream.Mon.Wea.Rev.,1981,109:2450～2463
[24]
丁一汇.高等天气学.北京:气象出版社,2005.138～149 Ding Yihui.Advanced Synoptic Meteorology (in Chinese).Beijing:China Meteorological Press,2005.138～149
