冬季中高纬500hPa高度和海表温度异常特征及其相关分析
CORRELATION IN MIDDLE AND HIGH LATITUDES BETWEEN WINTER SEA SURFACE TEMPERATURE AND 500 HPA GEOPOTENTIAL HEIGHT
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摘要: 用旋转主分量(RPC)方法,分析1948年到1988年40个冬季的中高纬500hPa高度场以及全球海表温度异常(SSTA)场的最主要的时空分布特征。然后通过交叉相关来讨论海气的同期相关特征。结果显示,冬季中高纬500hPa高度场最明显的异常型分别是太平洋北美型(PNA),西太平洋型(WP),西大西洋型(WA)以及东大西洋欧亚型(EAEU).冬季SSTA最明显的区域是赤道东太平洋(EEP)和赤道大西洋(EAL).其次是中纬度东北太平洋(NEP)及两大洋西部(NWP和NWA).中高纬度海气之间有很好的相关。与中高纬度500hPa高度场PNA型明显相关的是中高纬度东北太平洋(NEP)和赤道东太平洋(EEP)的SSTA.前者的强相关中心在中高纬;后者的强相关中心在中低纬。而与WA型明显相关的是中高纬度北大西洋的SSTA.中高纬度海气之间最强的相关在海气异常对应的空间位置上。而且这种区域性或邻域性的海气相关呈正相关,暖SSTA对应于正高度异常,冷SSTA对应于负高度异常。Abstract: The method of rotational principle component(RPC) was used to diagnose the temporaland spatial distributions in winter of the geopotential heightat 500 hPa and the sea surface temperature anomaly(SSTA) in the period from 1948 to 1988.Crossed-correlation was then used to study their correlation feature.Results not only confirmed the existence of the teleconnection patterns of the Pacific and North America(PNA) pattern, the western Pacific(WP) pattern,and the west Atlantic(WA) pattern in the geopotential height fidld as identitied by Wallace and Gutzlerin 1981 by using a different technic, but also found a new pattern(EAEU) which starts from the eastern Atlantic and crosses the Eurasian Continent.The mostsig nificant SSTA pattern in winteris associated with the SSTA in the eastern equatorial Pacific and equatorial Atlantic.This is followed by the mid-latitnde SST As on the northeast Pacific,western Pacific and western Atlantic.