南海登陆热带气旋对长江三角洲地区降水的影响
PRECIPITATION IN THE YANGTZE RIVER DELTA FIELDS CAUSED BY TROPICAL CYCLONES LANDING IN THE SOUTH CHINA SEA
-
摘要: 利用热带气旋年鉴资料统计了1949~2000年南海热带气旋影响期间我国长三角地区的最大降水量,计算有南海热带气旋影响时最大降水量大于50 mm的条件概率为60%。并把历年引起长三角地区50 mm以上降水的南海气旋频数序列作小波变换,发现其具有周期性振荡的特点,并且振荡周期在频率的分布上也有一定的规律。把南海热带气旋频数序列与夏季3个月副高面积指数之和的序列做交叉谱分析,发现两者具有准2年和准5年的耦合周期,气旋频数序列在位相上超前约半年。最后用1951~1999年的500 hPa月平均高度资料统计频数异常年的500 hPa高度场的距平和t统计量,发现在西太平洋、大西洋和极地都有显著的异常。Abstract: The maximum precipitation in the Yangtze River Delta which were caused by the tropical cyclones landing in the South China Sea in 1949—2000 were studied. The probability of precipitations above 50 mm was worked out when there was a tropical cyclone in the South China Sea. It is about 60 percents. A wavelet transform about the frequency of the tropical cyclones was performed. The results show that this series has notable oscillations and the periods vary in some regulations. As results of a cross power spectral analysis about the frequency series of the tropical cyclones and the sum series of the subtropical high area indexes of July, August and September, the two series have quasi-two-year and quasi-five-year coupled oscillations. The anomalies in the West Pacific, the Atlantic and the North Pole were found out when the Northern Hemisphere 500 hPa height data of anomalistic years were analyzed.
-
表 1 1949~2000年长三角地区降水与南海热带气旋的统计情况
表 2 历年引起长三角地区过程雨量大于50 mm的南海热带气旋的频数
表 3 南海热带气旋频数与副高面积指数交叉谱分析结果
-
[1] 任金声.南海登陆热带气旋与江淮出梅.气象, 1993, 19(3):25~28. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX199303005.htm [2] Chen L S. An overview on the interaction between tropical and mid-latitude weather systems. WMO/TD, No. 731, 1995.83~86. [3] Cheng Z H, Kang D, Chen L S, et al. Interaction between tropical cyclone and Meiyufront. ACTA Meteo Scinica, 1999, 13(1) :35~36. [4] 陈联寿, 徐祥德, 罗哲贤, 等.热带气旋动力学引论.北京:气象出版社, 2002. [5] 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.热带气象学报, 2001, 17(4):452~461. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200104014.htm [6] 魏凤英.现代气候统计诊断与预测技术.北京:气象出版社, 1999. [7] 黄嘉佑.气象统计分析和预报方法.北京:气象出版社, 2000. [8] 晁淑懿, 仇永炎.9608号台风登陆北上总能量变化及渤海高压维持.气象, 1998, 24(6):3~10. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX806.000.htm [9] 黄文根, 邓北胜, 熊廷南.一次台风暴雨的初步分析.应用气象学报, 1997, 8(2):247~251. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19970234&flag=1 [10] 蒋尚城.中低纬度系统的相互作用的特大暴雨.华北暴雨.北京:气象出版社, 1992. [11] 杜青文, 张迎新."96.8"特大暴雨的中尺度对流云团特征.气象, 1997, 23(10):39~43. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX710.008.htm [12] 江吉喜, 项续康."96.8"河北特大暴雨成因的中尺度分析.应用气象学报, 1998, 9(3):304~313. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19980344&flag=1 [13] 杨晓霞, 王景昌, 高留喜, 等.热带气旋大暴雨天气的初步分析.气象, 1997, 23(10):44-48. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX710.009.htm [14] 吴达铭, 雷小途.华东地区热带气旋汛频数异常时的环流分析.应用气象学报, 1999, 10(2):213~218. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19990260&flag=1 [15] 张卫青, 钱永甫.全球海气相互作用关键区及区内气候特征分析.热带气象学报, 2001, 17(1):23~33. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200101002.htm