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作 者:钱昌夏
出 处:《中国科学院上海天文台年刊》1995年第16期35-40,共6页Annals Shanghai Astronomical Observatory Chinese Academy of Sciences
摘 要:本文对瞬时极的移动速度用自回归谱估计的Marple算法进行了周期分析,结果表明,瞬时极的移动速度可能存在着2386.天(6.5年)、1168.9天(3.2年)、321.3天、163.7天、130.1天及92,7天等6个周期。同时计算了极移的振幅和周期,发现极移的速度与极移的振幅正相关,与极移的周期负相关。并且发现厄尔尼诺现象都出现在地极移动周期较短的年份。In this paper, the periods of velocity of polar motion are ana1ysed in using the meth0d ofMarple estimate. As a result, the periodic terms of 2386. S days, 1168. 9 days, 32l. 3 days,l63. 7 days, 13O. 1 days and 92. 7 days have been derived. By caloulating the amp1itude andthe period of polar motion, it is found that there is a positive correlation between the ve1ocityand the amplitude of polar motion, but a negative correlation between the velocity and theperiod of polar motion. It is also found that El N1fio is always happened in the year when theperiod of polar motion is short.
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