The ocean exerts a pervasive influence on Earth's environment. It is therefore important that
we learn how this system operates (NRC, 1998b; 1999). For example, the ocean is an …

Broadband ocean-bottom seismographs (BBOBSs) were first developed in the 1980s and
have since been used to explore the structure of Earth's interior beneath oceanic regions …

Plate tectonic theory hinges on the concept of a relatively rigid lithosphere moving over a
weaker asthenosphere, yet the nature of the lithosphere–asthenosphere boundary remains …

S‐to‐P (Sp) scattered energy independently confirms the existence of a seismic velocity
discontinuity at the lithosphere‐asthenosphere boundary that was previously imaged using …

Distributed acoustic sensing (DAS) is being explored in a variety of environments as a
promising technology for the recording of seismic signals in dense array configurations …

We present a new compilation and analysis of broad-band ocean bottom seismometer noise
properties from 15 yr of seismic deployments. We compile a comprehensive data set of …

After more than 10 years of the US ocean‐bottom seismometer (OBS) Instrument Pool
operations, there is still need for a consistent and accurate procedure to determine the …

Seismic noise in the period band 3–10 s is known as secondary microseism, and it is
generated at the ocean surface by the interaction of ocean gravity waves coming from nearly …

The primary goal of the Ocean Seismic Network Pilot Experiment (OSNPE) was to learn how
to make high quality broadband seismic measurements on the ocean bottom in preparation …

Physical sources of high‐frequency seismic noise in the ocean are investigated using data
from the Cascadia Initiative (CI) ocean bottom seismometer (OBS) network, hindcasts of …