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W. H. Munk. On the wind-driven ocean circulation. Journal of Meteorology, 1950, 7(2): 79-93.

被以下文章引用:

  • 标题: 春季北太平洋关键海域流场异常分析及其与夏季华北降水关系初探Analysis of Abnormal Spring Current in the Key Area of North Pacific and the Relationship with Summer Precipitation in North China

    作者: 卢姁, 汪鹏, 马佳, 王鑫

    关键字: 复EOF分析, 北太平洋, 华北地区CEOF Analysis; North Pacific; North China

    期刊名称: 《Climate Change Research Letters》, Vol.2 No.1, 2013-01-24

    摘要: 本文采用复EOF法,对春季北太平洋关键海域的上层洋流异常做了统计动力诊断,用以考察上层流场的年际和年代际变化,并简单讨论了其与夏季华北降水异常的关系。主要结论有:复EOF第一模态中,上层洋流异常表现为东北至西南走向的涡旋偶;时间系数有明显的年际和年代际变化,且与华北夏季降水的年际和年代际变化周期相似;在年代际尺度确定时,辐角的两个状态较好地对应于华北夏季降水的多寡;海洋西边界附近海水流动的异常是风应力异常所致,其性质属海洋Rossby波。In this paper, using CEOF analysis, the dynamic statistic diagnosis of abnormal upper current of springtime in the key area of North Pacific is done to discuss the inter-decadal and decadal variations of upper current and discover the relationship of summer precipitation in North China. The results are: In the first mode of CEOF, the abnormal upper current represents as a pair of vortices in the trend of EN to WS; there is obvious inter-decadal and decadal variation of time series, which is similar with the summer precipitation in North China; When decadal scale is identified, ampli-tudes’ two states are corresponding to the abnormal summer precipitation in North China; The abnormal of space field is caused by wind stress anomalies driving seawater off west coast, whose nature is ocean Rossby wave anomalies.

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