会议专题

按照两种类型理解70年代后期以来的ENSO型变化

ENSO.Another signature of the ENSO regime change is manifested by the frequentoccurrence of Warm-Pool (WP) type ENSO that accompanies SSTAs centered over thecentral Pacific near the WP edge and exhibits characteristics differing from those of CTENSO.The distinct manifestations of the two types of ENSO in this ENSO regimechange are identified clearly by removing the strong background decadal signal.Sincethe late 1970s,the WP ENSO features a weak eastward (westward) propagation of SSTAcenter in developing (decaying) phase,which makes no net contribution to the observedeastward propagation,and features a 2-3-yr period compared to the 4-5-yr period of theCT ENSO.Observations strongly suggest that WP and CT ENSO are independent quasi-biennial and quasi-quadrennial modes of the tropical Pacific climate variability,respectively,and that these two ENSO modes have coexisted actively since the late 1970swhen either El Nino or La Nina can be separated into the two types.

厄尔尼诺现象 南方涛动 海温异常 传播特征

任宏利 Fei-Fei JIN Malte F.STUECKER 谢瑞煌

国家气候中心,中国气象局气候研究开放实验室,北京 100081 国家气候中心,中国气象局气候研究开放实验室,北京 100081;Department of Meteorology,School of Ocean and Earth Sciences and Tec Department of Meteorology,School of Ocean and Earth Sciences and Technology,University of Hawaii,Hon 中国海洋大学气象系,青岛 266100

国内会议

第30届中国气象学会年会

南京

中文

1-15

2013-10-23(万方平台首次上网日期,不代表论文的发表时间)