张先恭, 赵汉光, 丁一汇. 1990: 1986-1987年尼厄诺期间太平洋海水水位的变化. 气象学报, (4): 424-432. DOI: 10.11676/qxxb1990.052
引用本文: 张先恭, 赵汉光, 丁一汇. 1990: 1986-1987年尼厄诺期间太平洋海水水位的变化. 气象学报, (4): 424-432. DOI: 10.11676/qxxb1990.052
Zhang Xiangong, Zhao Hanguang, Ding Yihui. 1990: SEA LEVEL FLUCTUATIONS IN THE PACIFIC DURING THE 1986-1987 EL NINO. Acta Meteorologica Sinica, (4): 424-432. DOI: 10.11676/qxxb1990.052
Citation: Zhang Xiangong, Zhao Hanguang, Ding Yihui. 1990: SEA LEVEL FLUCTUATIONS IN THE PACIFIC DURING THE 1986-1987 EL NINO. Acta Meteorologica Sinica, (4): 424-432. DOI: 10.11676/qxxb1990.052

1986-1987年尼厄诺期间太平洋海水水位的变化

SEA LEVEL FLUCTUATIONS IN THE PACIFIC DURING THE 1986-1987 EL NINO

  • 摘要: 本文根据太平洋海平面高度距平资料,分析了1986-1987年厄尼诺期间太平洋海水水位的变化,并与1982-1983年期间海水水位变化作了比较。证明海水水位不但对风场有很好的响应,而且还能较好地反映暖水团的移动,是监视ENSO事件的一种有效指标。文中还给出了厄尼诺事件不同发展阶段太平洋海平面高度距平分布的模型。

     

    Abstract: Based on the data of anomalies of monthly mean sea level of the Pacific ocean,the sea level fluctuations in the Pacific during the 1986-1987 El Nino are analyzed and compared with that in 1982-1983 counterpart.It is shown that the sea surface topography not only has a response to the wind field quite well,but also can better reflect the propagation of warm water mass.Therefore,the sea level is a effective indicator for monitoring ENSO event.An evolutive model of anomalies of monthly mean sea level in Pacific ocean at different phases of ENSO episode is given.

     

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