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亚洲热带地区对流爆发和推进的气候特征
引用本文:郭品文,朱乾根,刘宣飞. 亚洲热带地区对流爆发和推进的气候特征[J]. 南京气象学院学报, 1999, 22(3): 305-311
作者姓名:郭品文  朱乾根  刘宣飞
作者单位:南京气象学院大气科学系,南京,210044
摘    要:利用日本GMS TBB资料和GPCP降水资料,用滑动t-检验法研究了亚洲热带地区春夏季节转换期对流爆发和推进的气候特征。结果表明,亚洲热带地区对流爆发首先于4月中旬发生在中南半岛中部,然后向东缓慢推进。

关 键 词:突变  对流爆发  推进过程  滑动t-检验  亚洲季风

CLIMATOLOGICAL FEATURES OF CONVECTION ONSET AND ADVANCING OVER ASIAN TROPICAL REGION
Guo Pinwen,Zhu Qiangen,Liu Xuanfei. CLIMATOLOGICAL FEATURES OF CONVECTION ONSET AND ADVANCING OVER ASIAN TROPICAL REGION[J]. Journal of Nanjing Institute of Meteorology, 1999, 22(3): 305-311
Authors:Guo Pinwen  Zhu Qiangen  Liu Xuanfei
Abstract:Based on the T BB data from Japanese GMS satellite and the GPCP rainfall, movable t test technique is employed to reveal the climatological features of convection onset and advancing over the Asian tropical region during the spring to summer season.Results show that the convection occurs first in the middle Indo China peninsula in mid April,and then slowly advances eastward,expanding to the whole South China Sea in 28th pentad.The convection experiences such a strongly sbrupt change over Asian tropical area during the spring to summer season that the movable t test of the T BB and rainfall exceeds the statistical significance at 0.01 level.It is also found that each subregion has its own center of convection onset,with the northern South China Sea,northeastern Bay of Bengal and northeastern India being the most significant regions.
Keywords:TBB
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