南京大学学报(自然科学版) ›› 2010, Vol. 46 ›› Issue (3): 254260.
杜予罡, 储惠芸**
Du Yu Gang, Chu Hui Yun
摘要: 为研究环境因子对西北太平洋热带气旋气候特征的影响, 选取影响热带气旋( TC) 活动的 4 个单向环境因子: 海表温度、 850 hPa 气温、 对流层中低层比湿( 925~ 500 hPa) 和风速垂直切变( 200~
850 hPa), 海表温度只表征了海洋的加热状态, 而后 3个因子则只反映了大气的状态. 通过分析这 4 个环境因子与西北太平洋 T C 活动的相关关系, 进而定义两个指数: 考虑海气耦合作用的指数 -T (-T =SST - T a ,
其中 SST、 T a 分别为海表温度和 850 hPa 气温) 以及反映海洋上空湿空气稳定度的指数 - se ( se = se850 - se1 000 , 其中 se850 、 se1 000 分别表示 850hPa、 1000hPa 的假相当位温). 结果表明, 指数 -T 以
及 - se 与西北太平洋 TC 活动的相关性均比较显著, 其中考虑了海气耦合作用的指数 -T 能更好地表征TC 活动的气候变化.
[ 1 ]Gray W M . Global view of the origin of tropical disturbances and storms. Monthly Weather Re view, 1968, 96: 669~ 700. [ 2 ] Emanuel K A, Desautels C, Holloway C, et al. Environmental control of tropical cyclone intensity. Journal of the Atmospheric Sciences, 2004, 61: 843~ 858. [ 3 ] Zhu W J, Zhao K, Chen X M, et al. Separation of the environmental wind and typhoon by extended hurricane volume velocity processing method. Journal of Nanjing University (Natural Sciences) , 2010, 46( 3): 243~ 253. ( 朱文剑, 赵?坤, 陈小敏等. 用扩展飓风体积速度处理方法分离台风的环境平均风场. 南京大学学报( 自然科学), 2010, 46(3): 243~ 253) . [ 4 ] Emanuel K A. Thermodynamic control of hurricane intensity. Nature, 1999, 401: 665~ 669. [ 5 ] Chan J, Liu K S. Global warming and western North Pacific typhoon activity from an observational perspective. Journal of Climate, 2004, 17 (12) : 4590~ 4602. [ 6 ] Webster P J, Holland G J, Curry J A, et al. Change in tropical cyclone number, duration, and intensity in a warming environment. Science, 2005, 309: 1844~ 1846. [ 7 ] Chia H H, Ropelewski C F. The interannual variability in the genesis location of tropical cylones in the northwest Pacific. Journal of Climate, 2002, 15: 2934~ 2944. [ 8 ] Kurihara Y, Tuleya R E. A numerical simula tion study on the genesis of a tropical storm. Monthly Weather Review, 1981, 109: 1629~ 1653. [ 9 ] McBride J L, Zehr R M. Observational analysis of tropical cyclone formation. Part ∃: Comparison of non?developing versus developing systems. Journal of the Atmospheric Sciences, 1981, 38: 1132~ 1151. [ 10] DeM aria M, Kaplan J A. Statistical hurricane intensity prediction scheme (SHIPS) for the Atlantic Basin. Weather and Forecasting, 1994, 9: 209~ 220. [ 11] Holland G, Wang Y. What limits tropical cyclone intensity23 rd Conference on Hurricanes and Tropical M eteorology, Dallas, Texas, 1999, 955~ 958. [ 12] DeMaria M, Knaff J A, Connell B H. A tropical cyclone genesis parameter for the tropical Atlantic. Weather and Forecasting, 2001, 16: 219~ 233. [ 13] Hoyos C D, Agudelo P A, Webster P J, et al. Deconvolution of the factors contributing to the increase in global hurricane intensity. Science, 2006, 312: 94~ 97. [ 14] Zhao B, Duan Y H, Yu H, et al. A statistical analysis on the effect of vertical wind shear on tropical cyclone development. Acta M eteoro Sinica, 2006, 20: 383~ 388. [ 15] Bell G D, and Co ?authors. Climate assessment for 1999. Bulletin of the American Meteorological Society, 2000, 81: S1~ S50. |
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