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季飞, 支蓉, 龚志强, 等. 北太平洋高度场异常关联中心的空间结构特征的研究[J]. 大气科学, 2011, 35(4): 721-728. DOI: 10.3878/j.issn.1006-9895.2011.04.11
引用本文: 季飞, 支蓉, 龚志强, 等. 北太平洋高度场异常关联中心的空间结构特征的研究[J]. 大气科学, 2011, 35(4): 721-728. DOI: 10.3878/j.issn.1006-9895.2011.04.11
JI Fei, ZHI Rong, GONG Zhiqiang, et al. Analysis of Spatial Characteristics of Anomalous Correlation Centers in Height Fields of the North Pacific Ocean[J]. Chinese Journal of Atmospheric Sciences, 2011, 35(4): 721-728. DOI: 10.3878/j.issn.1006-9895.2011.04.11
Citation: JI Fei, ZHI Rong, GONG Zhiqiang, et al. Analysis of Spatial Characteristics of Anomalous Correlation Centers in Height Fields of the North Pacific Ocean[J]. Chinese Journal of Atmospheric Sciences, 2011, 35(4): 721-728. DOI: 10.3878/j.issn.1006-9895.2011.04.11

北太平洋高度场异常关联中心的空间结构特征的研究

Analysis of Spatial Characteristics of Anomalous Correlation Centers in Height Fields of the North Pacific Ocean

  • 摘要: 采用NCEP/NCAR全球高度场和地面气压资料, 研究了北太平洋负关联中心由低层到高层的空间分布, 以及与其有较强关联的异常关联中心的特征。结果表明, 各高度场中与北太平洋关联比较显著的中心比较一致, 主要分布在三个区域: 赤道中太平洋和白令海峡的负关联中心, 以及北美大陆东南部的正关联中心。三个区域内格点对北太平洋的综合作用表现为: 北太平洋区域在各层次高度场都存在明显的负关联中心, 体现出了一定正压结构特征, 并且中心的位置随着高度的增高在经向上有东移的特征, 在纬向上的移动则并不规则。就三个异常关联中心而言, 对北太平洋区域影响最显著的区域在700 hPa、 500 hPa和200 hPa高度场都是位于赤道中太平洋的负关联中心, 在地面气压场中则是位于白令海峡的负关联中心。最先影响北太平洋区域的在地面气压和700 hPa高度场是位于北美大陆东南部的正关联中心, 在500 hPa和200 hPa高度场是位于赤道中太平洋的负关联中心, 因此, 在不同高度场, 对于北太平洋首要关注的影响区域应区别对待。

     

    Abstract: The distribution of negative correlation center in the North Pacific Ocean from the low level to high level and characteristics of other anomalous centers which have strong correlations with the North Pacific Ocean are analyzed using the NCEP/NCAR global height field data and surface pressure data. Research results show that the distributions of the centers which have remarkable correlations with the North Pacific Ocean are always the same in each height field, and the three correlation centers are: negative centers in the central equatorial Pacific and the Bering Strait, positive center in the southeast of the North America continent. The correlations between grid points in the North Pacific Ocean and grid points in these three centers show that there is an obvious negative correlation center in the North Pacific Ocean at each height which reflects a character of barotropic structure, and the negative center moves eastward with the height increasing in the meridional direction while the ambulation in the zonal one is irregular; in these anomalous centers, the most remarkable center at 700 hPa、 500 hPa, and 200 hPa which influences the the North Pacific Ocean is the negative center in the central equatorial Pacific while that in the surface pressure field is the negative center in the Bering Strait. The correlation center first influencing the North Pacific Ocean is the positive one in the southeast of the North America continent for surface pressure and 700 hPa, and is the negative one in the central equatorial Pacific at 500 hPa and 200 hPa.

     

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