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黑潮弯曲时的北太平洋冬季海温异常对大气低频振荡的影响
引用本文:李薇,刘秦玉,徐启春.黑潮弯曲时的北太平洋冬季海温异常对大气低频振荡的影响[J].中国海洋大学学报(自然科学版),1994(4).
作者姓名:李薇  刘秦玉  徐启春
摘    要:利用中科院大气物理研究所开放实验室IAP-AGCM(二层大气环流模式),针对黑潮弯曲时的北太平洋冬季表层海温(SST)异常进行八个月的数值积分试验。试验结果表明:黑潮弯曲时北太平洋冬季SST异常对大气低频振荡的影响具有明显的30-60d振荡的特征;在北半球的30-60d振荡,大部分地区为向西传播,在南半球则为向东传播;其经向传播较为复杂,在120°E剖面上以向南传播为主;热带地区受此SST异常的影响以西太平洋、印度洋大气加热场的30-60d振荡为主要标志。

关 键 词:北太平洋  黑潮弯曲  冬季  海温异常  低频振荡

THE EFFECT OF THE SST ANOMALY IN THE NORTH PACIFIC DUE TO THE MEANDER OF THE KUROSHIO IN WINTER ON THE LOW FREQUENCY OSCILLATION
Li Wei, Liu Qinyu, Xu Qichun.THE EFFECT OF THE SST ANOMALY IN THE NORTH PACIFIC DUE TO THE MEANDER OF THE KUROSHIO IN WINTER ON THE LOW FREQUENCY OSCILLATION[J].Periodical of Ocean University of China,1994(4).
Authors:Li Wei  Liu Qinyu  Xu Qichun
Institution:Institute of Physical Oceanography
Abstract:A numerical integration experiment was carried out on the Sea Surface Temperature (SST) anomaly in the North Pacific corresponding to the meander of the Kuroshio in winter(January-March) by using a two-layer global atmospheric general circulation model (IAP-AGCM). The experiment showed that the SST anomaly in the North Pacific in winter could induce a 30- 60 day oscillation in the global atmosphere. The direction of the oscillation propagation along the latitude and the longitude is different in different hemispheres. In the tropical zone, the 30- 60 day oscillation of the atmospheric heating field is induced. The low frequency oscillation affects the global circulation through a 2-dimensional Rossby wave train.
Keywords:North Pacific  meander of the Kuroshio  winter  SST anomaly  low frequency oscillation  
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