Seismic sea wave of April 1, 1946, as recorded on tide gages
Seismic sea wave of April 1, 1946, as recorded on tide gages
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验潮仪记录的 1946 年 4 月 1 日海啸
DOI：
10.1029/tr027i004p00490
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发表时间：
1946
期刊：
影响因子：
--
通讯作者：
C. K. Green
中科院分区：
文献类型：
--
作者：
C. K. Green
本文分析了东太平洋从北纬57°到南纬33°的20个验潮站记录的1946年4月1日地震海浪的爆发。走时曲线，计算公式V =，示出是在良好的协议与观测到的时间的地震海浪的到达。最初的上升和随后的下降的平均比率被发现是1比3，这可能是目击者经常提到最初的衰退的原因。第一个半周期是作为测量地震海浪的周期而得出的，平均为15.6分钟。距离较近的站的平均周期为15.0分钟，而距离较远的站的平均周期为17.4分钟。
Records from some 20 tide stations in the eastern Pacific Ocean, covering a stretch from 57°N latitude to 33°S latitude, which show the onset of the seismic sea wave of April 1, 1946, are analyzed. Travel-time curves, computed from the formula V = , are shown to be in good agreement with the observed times of arrival of the seismic sea wave. The average ratio of initial rise to succeeding fall of the water is found to be one to three, which may account for the frequent mention of an initial recession by eyewitnesses. The first half period is derived as a measure of the period of the seismic sea wave which is found to average 15.6 minutes. The period for the nearer stations averages 15.0 minutes, while for the farther stations it averages 17.4 minutes.