Nino C区秋季海温异常对东亚冬季大气环流的影响
POSSIBLE IMPACTS OF NINO C SSTA ON WINTER ATMOSPHERIC GENERAL CIRCULATION OVER EAST ASIA
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摘要: 研究了秋季赤道中东太平洋(Nino C区:0~10°S,180~90°W)的SST异常对东亚冬季大气环流的可能影响。在揭示二者联系的基础上,通过分析海温异常所引起的500hPa高度、经向风及纬向风的异常特征,探讨了秋季海温异常影响东亚冬季大气环流的可能途径。研究发现,Nino C区秋季SST异常,能够对东亚及西太平洋地区的大气环流及风场产生显著影响,进而影响东亚冬季风活动:秋季SST正(负)异常,引起西太平洋地区出现类似负(正)WP遥相关型的环流异常,中纬度纬向西风加强(减弱),东亚及沿海地区出现异常南(北)风分量,经向风减弱(加强),最终导致偏弱(强)的东亚冬季风活动。这是海温异常影响东亚冬季大气环流的一种可能途径。Abstract: In this paper, possible impacts of equatorial east-central Pacific (Nino C) SSTA on winter atmospheric general circulation over East Asia are investigated. The relationship between them is disclosed and the possible mechanism of SSTA influencing winter atmospheric general circulation is discussed by investigations on the anomalous features of 500 hPa circulation, zonal and longitudinal winds induced by SSTA. Results show that Nino C SSTA has significant impacts on atmospheric general circulation and winds over East Asia and West Pacific, that is, positive SST anomaly in Autumn can lead to atmospheric circulation anomalies that are similar to negative WP pattern over the Western Pacific, in such a way that the mid-latitude zonal westerly intensify and meridional wind anomalies appear over East Asia and its adjoining sea decrease with anomalous south wind component, and the activities of East Asian winter monsoon weaken. It is a possible mechanism by which SSTA affects winter atmospheric general circulation.
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[1] 符淙斌,孙翠霞,张金枝.赤道海温异常与大气垂直环流圈[J].大气科学,1979,3:50-57. [2] 吴国雄,CUBASCH U.El Nino海温异常对纬项平均经向环流及大气输送特征的影响[J].中国科学B,1986,第10期:1109-1120. [3] 李崇银,胡季.东亚大气环流与El Nino相互影响的一个分析研究[J].大气科学,1987,11:359-364 [4] 吴正贤,李崇银,陈彪,等.1982-1983年冬季厄尔尼诺期间大气环流异常的诊断分析[J].热带气象,1990,6: 253-264. [5] 蒋全荣,WALLACE J M.冬半年北半球太平洋地区的海气相互作用及其遥相关[J].海洋学报,1991,13: 621-628. [6] 朱乾根,谢立安.1986-1987年北半球冬季亚澳地区大气环流异常及其与太平洋SST异常的联系[J].热带气象,1988,4: 254-262. [7] 李崇银.中国东部地区的暖冬与厄尔尼诺[J].科学通报,1989,33: 283-286. [8] 郭其蕴,王日昇.东亚冬季风活动与厄尔尼诺的关系[J].地理学报,1990,45: 68-77. [9] 陶诗言,张庆云.亚洲冬夏季风对ENSO事件的响应[J].大气科学,1998,22: 399-407. [10] 穆明权,李崇银.东亚冬季风年际变化的ENSO信息[J].大气科学,1999,23: 276-285. [11] 施能,朱乾根.北半球冬半年遥相关型强度指数的年际变化特征及其与厄尔尼诺的遥响应[J].南京气象学院学报,1993,16: 130-137. [12] 吴洪宝.我国冬季气温异常与北半球500 hPa大气环流遥相关的关系[J].南京气象学院学报,1993,16: 115-119. [13] ENSO监测小组.厄尔尼诺事件的划分标准和指数[J].气象,1989,15: 37-38. [14] WALLACE J M,GUTZLER D S.Teleconnections in the geopotential height field during the northern hemisphere winter[J].Mon Wea Rev,1981,109: 784-812.
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