中国汛期降水的印度洋SSTA信号特征分析
THE SSTA SIGNAL CHARACTERISTIC ANALYSIS OVER INDIA OCEAN DURING FLOOD SEASON IN CHINA
-
摘要: 用EOF和CCA方法研究了印度洋海表温度距平场与中国汛期降水场的遥相关分布特征,结果表明:印度洋SSTA场与中国汛期降水场相关明显,海温场异常分布对中国汛期南北经向雨带的变化及中国西北、西南和长江黄河下游地区汛期旱涝的影响明显,揭示了中国汛期旱涝异常分布的印度洋海温变化的强信号现象,说明特定的印度洋海温分布可以作为中国汛期旱涝预报的强信号因子。Abstract: The teleconnection distribution characteristics between sea surface temperature (SST) over India Ocean and the precipitation during rainy season in China were studied by using the method of EOF and CCA. The results indicated that the change of SST field will affect the change of rain belt during rainy seasons in China,and heavily affect the precipitation in north-west,south-west,the Yangzi and Yellow River downstream in China. The strong signal phenomena of SSTA over India Ocean were revealed and it showed that the precipitation during rainy season in China may be forecasted by analyzing SST distribution characteristics over India Ocean.
-
[1] 苗秋菊,徐祥德.区域性旱涝与海温特征分布的相关链模型[J].应用气象学报(增刊),1998,9:47-56. [2] 陈隆勋,朱乾根,罗会邦,等.东亚季风[M].北京:气象出版社,1991.204-209. [3] 黄荣辉,孙凤英.热带西太平洋暖池的热状态及其上空的对流活动对东亚夏季气候异常的影响[J].大气科学,1994,18:141-151. [4] 罗绍华,金祖辉.南海海洋温度变化与初夏西太平洋副高活动及长江中下游汛期降水关系的分析[J].大气科学,1986,10:409-417. [5] 金祖辉,沈如桂.长江中下游旱梅和涝梅年海温场及大气环流系统的特征[A].气象科学技术集刊(11)[C].北京:气象出版社,1987.83-88. [6] 严华生,王学仁.多因变量及要素场统计预报[M].北京:气象出版社,1991.36-41. [7] 李崇银.东亚冬季风异常与ENSO[A].气候变化若干问题研究[C].北京:科学出版社,1992.87-97. [8] 李崇银.频繁强东亚大槽活动与El Nino的发生[J].中国科学(B),1998,18: 667-674. [9] 罗绍华,金祖辉,陈烈庭.印度洋和南海海温与长江中下游夏季降水的相关分析[J].大气科学,1985,9: 336-342. [10] 郭其蕴,王继琴.中国与印度夏季风降水的比较研究[J].热带气象,1988,4: 53-60. [11] 魏凤英.全球海表温度变化与中国汛期降水异常分布[J].应用气象学报,1998(增刊):100-108. [12] 晏红明,肖子牛.EL Nino位相期间印度洋SSTA对亚洲季风及中国南部初夏降水影响的数值模拟研究[J].大气科学,2001,待刊.
点击查看大图
计量
- 文章访问数: 1001
- HTML全文浏览量: 0
- PDF下载量: 1017
- 被引次数: 0