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Deep-Ocean Measurements of Tsunami Waves

机译:海啸的深海测量

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Deep-ocean tsunami measurements play a major role in understanding the physics of tsunami wave generation and propagation, and in improving the effectiveness of tsunami warning systems. This paper provides an overview of the history of tsunami recording in the open ocean from the earliest days, approximately 50 years ago, to the present day. Modern tsunami monitoring systems such as the self-contained Deep-ocean Assessment and Reporting of Tsunamis and innovative cabled sensing networks, including, but not limited to, the Japanese bottom cable projects and the NEPTUNE-Canada geophysical bottom observatory, are highlighted. The specific peculiarities of seafloor longwave observations in the deep ocean are discussed and compared with observations recorded in coastal regions. Tsunami detection in bottom pressure observations is exemplified through analysis of distant (22,000 km from the source) records of the 2004 Sumatra tsunami in the northeastern Pacific.
机译:深海海啸测量在了解海啸波产生和传播的物理原理以及提高海啸预警系统的有效性方面发挥着重要作用。本文概述了从大约50年前的最早的日子到现在的公海海啸记录的历史。重点介绍了现代海啸监测系统,例如独立的海啸深海评估和报告以及创新的有线传感网络,包括但不限于日本海底电缆项目和NEPTUNE-加拿大地球物理海底观测站。对深海中海底长波观测的特殊性进行了讨论,并与沿海地区记录的观测结果进行了比较。通过分析东北太平洋2004年苏门答腊海啸的遥远记录(距震源22,000 km)来举例说明海底压力观测中的海啸检测。

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