Microseisms and ocean wave measurements

Microseisms and ocean wave measurements
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DOI:
10.1109/48.740159
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发表时间:
1999
影响因子:
4.1
通讯作者:
C. Tindle;M. Murphy
C. Tindle;M. Murphy
中科院分区:
工程技术2区
文献类型:
--
作者:
C. Tindle;M. Murphy

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研究人员将新西兰奥克兰的微震测量结果与新西兰西海岸(位于奥克兰西南约150公里处)的海浪数据进行了比较。大多数时候都有很强的相关性。例外情况是,奥克兰地区受到东风的强风的影响。奥克兰0.05-1赫兹波段的微震活动似乎完全是由海浪引起的。
Measurements of microseisms in Auckland, New Zealand, are compared with ocean wave data taken on the west coast of New Zealand, about 150 km southwest of Auckland. There is strong correlation at most times. Exceptions are when the Auckland area is subject to strong winds from the easterly quarter. Microseism activity in Auckland in the 0.05-1-Hz band appears to be entirely due to ocean waves.