印度洋-太平洋各季海温年际变异模的相关性及其与我国夏季降水的关系
LINKAGE BETWEEN THE INTERANNUAL VARIATION PATTERNS OF SEASONAL SST IN INDIAN OCEAN-PACIFIC AND THEIR RELATIONSHIP WITH THE SUMMER RAINFALL OVER CHINA
-
摘要: 用1958~1998年NCEP再分析资料、Reynolds海温及中国160站月降水资料分析了印度洋-太平洋不同季节海温年际变异的主要空间分布特征以及它们之间的相互联系,探讨了夏季亚澳季风区海温异常型与我国夏季降水的关系。结果表明:冬季印度洋-太平洋海温年际变化的第一模态与随后春季的第一模态、夏秋季亚澳季风区的海温异常型(第二模态)有非常显著的相关关系,即如果冬季海温异常为ElNiño(La Niña)型,则其后的春季也为ElNiño(LaNiña)型,而随后的夏、秋季在亚澳季风区的热带海温有暖(冷)异常。夏季亚澳季风区海温异常与我国长江中游至江南的夏季降水有显著的正相关,即夏季亚澳季风区热带海温暖(冷)异常对应长江中游及江南的夏季降水偏多(少)。与东亚冬季风异常有关的冬季北太平洋海温异常型,可以通过与夏季亚澳季风区海温的异常有显著相关性进而影响到东亚夏季风。Abstract: Linkage between the interannual variation patterns of seasonal sea surface temperature(SST) in Indian ocean-Pacific and their relationship with the summer rainfall over China are investigated,using the NECP reanalysis data,Reynolds SST and the station rainfalls in China from 1958 to 1998.There exist significant correlation between the dominant mode of SST anomalies in winter(ENSO mode) based on EOF analysis and the dominant mode of SST in following springs,the anomalous modes of SST in Asian-Australian monsoon area in following summers and autumns.It means that when the El Nino(La Nina)-like anomalous pattern of SST occurs in winter in Indian ocean-Pacific,followed by the El Nino(La Nina)-like anomalous pattern of SST in the coming spring,then the positive(negative) anomalous mode of SST appears in the tropical ocean within the Asian-Australian monsoon area in the summer and autumn to come.The anomalous mode of SST in the tropical Asian-Australian monsoon area has significant positive correlation with the summer rainfall over the middle reach of the Yangtze River and the vicinity south to it.The anomalous SST mode in winter in the north Pacific,which is closely related with the anomalous East Asian winter monsoon,may make an impact on the East Asian summer monsoon through its close connection with the summer anomalous mode of SST in the tropical Asian-Australian monsoon area.
-
Key words:
- Indian ocean-Pacific /
- sea surface temperature /
- interannual variation /
- summer rainfall
-
[1] LUO H B.Effect of winter monsoon on summer monsoon through air-sea interaction[J].Acta Meteorologica Sinica,1995,9(1):26-33. [2] 陈隽,孙淑清.东亚冬季风异常与全球大气环流变化I:强弱冬季风影响的对比研究[J].大气科学,1999,23(1):101-111. [3] 孙淑清,陈隽.异常东亚冬季风对夏季南海地区风场及热力场的影响[J].气候与环境研究,2000,5(4):400-416. [4] CHEN W,GRAF H F,HUANGR H.The interannual variability of East Asian winter monsoon and its relation to the summer monsoon[J].Adv AtmosSci,2000,17(1):46-60. [5] 陶诗言,朱文姝,赵卫.论梅雨的年际变异[J].大气科学,1988(特刊):13-21. [6] HUANG R H,WU Y F.The influence of the ENSO on the summer climate in China and its mechanism[C]//Proleedingsof Japan-U S,Workshop on theEl Nino Southern Oscillation Phenomenon.Tokyo:Tokyo University,1987:10-15. [7] WEARE B C,SOONG A.Empirical orthogonal analysis of Pacific sea surface temperature[J].J Phys Ocean,1976,6(4):671-678. [8] 张启龙,温学传,颜廷状.西太平洋暖池海域SST场的时空特征[J].海洋与湖沼,2001,23(4):349-354. [9] RASSMUSSON E N,CARPENTER T N.Variations in tropical sea surface temperature and surface wind field associated with the SouthernOscillation/El Nino[J].Mon Wea Rev,1982,110(5):354-384. [10] PHILANDER S G H.El Nino Southern Oscillation phenomena[J].Nature,1983,302:296-301. [11] WANG Y F,WANG B,OH J H.Impact of the Preceding El Nino on the East Asian summer atmosphere circulation[J].J Meteo Soc Japan,2001,79(1B):575-588. [12] 赵永平,陈永利.两类ENSO事件前期的热带太平洋海温距平场[J].热带气象学报,1998,14(3):226-232. [13] 徐建军,朱乾根.印度洋-太平洋海温长期变化的周期性及其年代际变化[J].热带气象学报,1998,14(4):353-358. [14] 彭勇刚,简茂球,梁巧倩,等.印度洋-太平洋海表温度异常的持续性特征[J].中山大学学报(自然科学版),2004,43(3):90-94. [15] 李清泉,赵宗慈.1997/1998年热带太平洋海温异常的诊断分析与预报检验[J].热带气象学报,2001,17(4):355-363. [16] 黄嘉佑.气象统计分析与预报方法[M].北京:气象出版社,2000:222-226. [17] 陈文.El Ni(n)o和La Ni(n)a事件对东亚冬、夏季风循环的影响[J].大气科学,2002,26(5):595-610. [18] KLEIN S A,SODEN B J,LAU N C.Remote sea surface temperature variations during ENSO:Evidence for a tropical atmospheric bridge[J].J Climate,1999,12(4):917-932. [19] 曹杰,董慧林,陶云.热带印度洋和热带太平洋海温振荡规律的研究[J].热带气象学报,2003,19(1):9-16. [20] HSU H H,CHEN Y L,KAU W S.Effect of atmosphere-ocean interaction on the interannual variability of winter temperature in Taiwan and EastAsia[J].Climate Dynamics,2001,17(4):305-316.
点击查看大图
计量
- 文章访问数: 1155
- HTML全文浏览量: 0
- PDF下载量: 988
- 被引次数: 0