西北太平洋台风活动的年代际变化与大尺度环流因子的关系
LARGE SCALE CIRCULATION ASSOCIATED WITH INTERDECADAL VARIATIONS OF TYPHOON ACTIVITY OVER THE WESTERN NORTH PACIFIC
-
摘要: 用多项式拟合和统计分析的方法对1960~2005年西北太平洋台风年频数资料进行分析表明:台风活动存在明显的年代际变化,46a间台风活动存在两个高频期和两个低频期,高低频期台风频数的差异主要集中在7~10月(称为台风活跃季),利用台风活跃季的NCEP/NOAA资料对影响台风年代际变化的大尺度环流因子进行分析,结果表明:与低频期相比,在台风生成的高频期出现了较高的海表温度、较低的海平面气压、较大的高层散度和低层相对涡度、较小的垂直风切变,而且500hPa风场利于台风的生成和向西北太平洋移动,西太平洋副热带高压偏北,100hPa南亚高压偏弱。西北太平洋海盆的总降水量的年代际变化与台风的年代际变化关系不明显。Abstract: Based on the Typhoon(TY) frequency data of Tropical Cyclone Yearbooks from 1960 to 2005,TY frequency of 46a has exhibited obvious decadal-scale variability by the polynomial fit and statistical analysis.And it has two high frequency periods(HFP) and two low frequency periods(LFP).Significant differences in the number of TYs between HFP and LFP are found in the TY activity season from July through October.Differences of large-scale circulation during HFP and LFP are investigated with NCEP/NOAA data of TY activity season.In HFP,the condition includes not only high sea surface temperature,low sea level pressure,large divergence of upper air,large relative vorticity of low level and small vertical shear,but also favorable 500-hPa wind vector for TY activity and movement to western North Pacific,northward positions of the subtropical anticyclone over the western Pacific,and a South Asian anticyclone at 100hPa much smaller than in LFP.The precipitation of western North Pacific has no clear influence on TY activity.
-
Key words:
- Western North Pacific /
- typhoon /
- frequency /
- interdecadal variation /
- large-scale circulation
-
[1] 阎俊岳,张秀芝,李江龙.135°E以西西北太平洋热带气旋迅速加强的气候特征[J].热带气象学报,1997,13(4):297-305. [2] 陈敏,郑永光,陶祖钰.近50年(1949~1996)西北太平洋热带气旋气候特征再分析[J].热带气象学报,1999,15(1):10-16. [3] 钱燕珍.近120年西北太平洋及其登陆中国的热带气旋统计分析[J].浙江气象,2004,25(2):6-9 [4] CHAN Johnny,LIU Kinsik.Global Warming and Western North Pacific Typhoon Activity from an Observational Perspective[J].Journal of Climate,2004,17(12):4 590-4 602. [5] 林慧娟,张耀存.影响我国热带气旋活动的气候特征及其与太平洋海温的关系[J].热带气象学报,2004,20(2):218-224. [6] GRAY W M,SHEAFFER J D.El Nino and QBO influences on tropical cyclone activity[M] //Teleconnections linking worldwide climate anomalies.Cambridge:Cambridge University Press,1991:257-284. [7] LANDERSEA C W,BELL G D,GARY W M,et al.The extremely active 1995 Atlantic hurricane season:Environmental conditions and verificationof seasonal forecasts[J].Mon Wea Rev,1998,12(6):1 174-1 193. [8] CHU P S.Large-scale Circulation Features Associated with Decadal Variations of Tropical Cyclone Activity over the Central North Pacific[J].Journal of Climate,2002,15(9):2 678-2 689. [9] YUMOTO,TOMONORI M.Interdecadal Variability of Tropical Cyclone Activity in the Western North Pacific[J].Journal of the MeteorologicalSociety of Japan,2001,79(1):23-35. [10] FRANK W M.Tropical Cyclone Formation[M] //A global view of tropical cyclones.Chicago:University of Chicago Press,1987:53-90. [11] 张光智,张先恭,魏凤英.近百年西北太平洋热带气旋年频数的变化特征[J].热带气象学报,1995,11(4):315-323. [12] 叶英,董波.西北太平洋强热带气旋活动的年代际变化[J].气象,1998,24(7):29-34. [13] 张庆云,彭京备.夏季东亚环流年际和年代际变化对登陆中国台风的影响[J].大气科学,2003,27(1):97-106. [14] 中国气象局.台风年鉴(1960~1988年)[Z].北京:气象出版社,1960~1989. [15] 中国气象局.热带气旋年鉴(1989~2005年)[Z].北京:气象出版社,1990~2006. [16] 雷小途,陈联寿.热带气旋与中纬度环流系统相互作用的研究进展[J].热带气象学报,2001,17(4):452-462. [17] LAU K M,WENG H.Interannual,Decadal,Interdecadal and Globaal Warming Signals in Sea Surface Temperature during 1955-1997[J].J Climate,1999,12(6):1257-1267.
点击查看大图
计量
- 文章访问数: 1029
- HTML全文浏览量: 0
- PDF下载量: 1071
- 被引次数: 0