Marie C. Eblé

TL;DR: In this article, the authors discuss the scientific need for globally integrated deep-ocean observing, its status, and the key scientific questions and societal mandates driving observing requirements over the next decade.

TL;DR: In this article, the authors provide an overview of the history of tsunami recording in the open ocean from the earliest days, approximately 50 years ago, to the present day, and present day modern tsunami monitoring systems such as the self-contained Deep Ocean Assessment and Reporting of Tsunamis and innovative cabled sensing networks.

TL;DR: In the early 1980s, the United States National Oceanic and Atmospheric Administration Pacific Marine Environmental Laboratory established the fundamentals of the contemporary tsunameter network deployed throughout the world oceans.

TL;DR: In this article, the authors examined the seismic surface waves generated by earthquakes and found that they produced BP fluctuations in response to the vertical bottom acceleration induced as the waves propagated along the water-bottom interface.

TL;DR: Watada et al. as discussed by the authors presented leading negative phase signatures in examples from the more than 40 deep-ocean bottom pressure and approximately 200 tide gauge records investigated for this study.