登陆我国过湖泊热带气旋的统计特征
STATISTICAL CHARACTERISTICS OF TROPICAL CYCLONES MAKING LANDFALLS AND PASSING THROUGH LAKES IN CHINA
-
摘要: 利用1949～2001年热带气旋年鉴资料,对53年登陆我国并经过内陆湖泊的热带气旋特征进行统计分析。结果表明:登陆过湖泊热带气旋在陆上维持时间长,登陆时强度较强;湖泊地带能延缓登陆TC强度的衰减;热带气旋经过内陆湖泊时大多表现为中心气压维持不变或降低,风速增大;长江中游地区是登陆过湖泊热带气旋消失数最多的区域。Abstract: By using 53-year tropical cyclone(TC) Yearbooks data from 1949 to 2001,statistical analyses are performed to study the climatic features of landing TCs through lakes in China. Results show that those TCs can sustain long time inland and the intensity is very strong during the landfall. The lake can noticeably reduce decay due to landfall,with the minimum pressure mostly maintained or decreased and the maximum velocity increased. The middle reach of the Yangtze River has the biggest TC dissipating rate as compared with the other TC activity areas.
-
Key words:
- tropical cyclone /
- landfall /
- lake /
- statistic
-
[1] 陈联寿.台风登陆问题研究的进展[C] //第十一届全国热带气旋科学讨论会论文摘要文集.北京:中国气象科学研究院,1999:11-12. [2] SHEN Weixing,ISAAC Ginis.A numerical investigation of land surface water on landfalling hurricanes[J].J Atmos Sci,2002,59(4):789-802. [3] 陈联寿,丁一汇.西太平洋台风概论[M].北京:科学出版社,1979:423-428;466-474. [4] 钟元,余晖,王东法.环境场对东海登陆热带气旋陆地路径的影响[J].热带气象学报,2006,22(4):313-320. [5] 张胜军.台风结构动力学模型及其数值试验[D] //博士研究生学位论文.北京:中国气象科学研究院,2002:39-40. [6] 李英,陈联寿,张胜军.登陆我国热带气旋的统计特征[J].热带气象学报,2004,20(1):14-23. [7] CHARLES E,KONRAD I I.Diurnal variations in the landfall times of tropical cyclones over the Eastern United States[J].Mon Wea Rev,2001,129(10):2 627-2 631. [8] 梁建茵.登陆我国热带气旋登陆时间日变化特征分布[J].热带气象学报,2003,19(增刊):160-165. [9] 刘春霞.广东热带气旋年际变化的小波分析[J].热带气象学报,2001,17(4):381-390. [10] 谢炯光,纪忠萍.登陆广东省热带气旋的奇异谱分析[J].热带气象学报,2003,19(2):163-168. [11] 中国气象局.台风年鉴(1971～1988年)[Z].北京:气象出版社,1972-1989. [12] 中国气象局.热带气旋年鉴(1989～2000年)[Z].北京:气象出版社,1990-2001. [13] 陈联寿,徐祥德,罗哲贤,等.热带气旋动力学引论[M].北京:气象出版社,2002:251;300-310. [14] 王晓芳,李红莉.登陆我国热带气旋的气候特征[J].暴雨·灾害,2007,26(3):251-255. -
点击查看大图
计量
- 文章访问数: 966
- HTML全文浏览量: 2
- PDF下载量: 944
- 被引次数: 0
下载:
粤公网安备 4401069904700003号