摘要
利用长江中下游1954—2001年梅雨量资料和NCEP/NCAR 1954—2001年逐日高度场、风场、比湿场和地面气压场资料,采用EOF分解、合成分析、SVD分解等方法,详细讨论了北太平洋大气热源与长江中下游梅雨的关系。结果表明:西北太平洋大气热源与长江中下游梅雨量存在显著负相关,东太平洋大气热源与长江中下游梅雨量存在显著正相关,通过信度为95%的Monte-Carlo检验,具体表现为当菲律宾群岛附近洋面、西太平洋暖池区及西北太平洋西风飘流区大气热源异常增加(减少)时,赤道中东太平洋大气热源异常偏低(偏高),会造成长江中下游梅雨异常偏少(偏多),反之亦然,合成分析、点相关分析和SVD的分析结果完全一致。
Based on the precipitation of Meiyu at 25 stations of mid-lower reaches of the Yangtze and the daily re- analysis geopotential height, wind field, humidity field and surface pressure field data （2.5°× 2.5°） from 1954 to 2001, the relationship between the atmospheric heat source in the North Pacific Ocean and the ab- normality of Meiyu precipitaion of mid-lower reaches of the Yangtze is investigated in terms of the Z index methold, empirical orthogonal function（EOF）, composite analysis, singular value decomposition （SVD）, and so on. The results of Z index methold indicate that there are notable multi （shored） Meiyu precipitation on mid-lower reaches of the Yangtze during the Meiyu period. There are 8 years in which the Meiyu precipita- tion is abnormally more and 6 years in which the Meiyu precipitation is abnormally less. The first mode of EOF shows the ENSO mode of the atmospheric heat source of North Pacific Ocean on mid-lower reaches of the Yangtze during the Meiyu period which express specifically the positive （negative） correlation between the atmospheric heat source in the mid-east Pacific Ocean and the north Pacific Ocean. The second mode of EOF shows the abnormal mode of the atmospheric heat source on the mid-lower reaches of the Yangtze during the Meiyu period which represents specifictly the positive （negative） correla- tion between the atmospheric heat source in the equatorial Pacific Ocean and the north Pacific Ocean of the middle-high latitudes. The results of SVD show that there are notable correlation between the Meiyu precipitation in the good（poor） Meiyu year and the atmospheric heat source in the Pacific Ocean. Through Monte-Carlo test at 95%, it shows there is positive （negative） correlation between the atmospheric heat source in the western （eastern） Pacific Ocean and the precipitation on mid-lower reaches of the Yangtze. When the SSTA around the Philippine island ocean and in the north-west Pacific Ocean are marked increas- ing（decreasing）, convective activity is vigorous （weaken）, the atmospheric heat in the north-west Pacific Ocean is increasing（decreasing）, so the atmospheric heat in the eastern Pacific Ocean is decreasing（increas- ing）, while the precipitation is marked increasing（decreasing） on mid-lower reaches of Yangtze river, and vice verse. The results of composite analysis and correlation analysis and SVD are identical congruent.
出处
《应用气象学报》
CSCD
北大核心
2009年第2期240-246,共7页
Journal of Applied Meteorological Science
基金
国家自然科学基金项目(40675036)
中国气象局成都高原气象研究所基本科研项目(BROP200708)
成都信息工程学院科研基金项目(CRF200801)共同资助
关键词
梅雨
大气热源
Z指数
EOF
SVD
Meiyu
atmospheric heat source
Z index method
EOF
SVD
