Comparison of the ambient noise data recorded at near‐coastal ocean bottom and inland
seismic stations at the Oregon coast with both offshore and nearshore buoy data shows that …

Compressional (P)-wave attenuation, shear (S)-wave attenuation, and shear (S)-wave
velocity measurements, compiled for fine-grained, unconsolidated sediments, show trends …

This article discusses inversions for bottom geoacoustic properties using broadband
acoustic signals obtained from explosive sources. Two different inversion schemes for …

Ice-covered ocean worlds possess diverse energy sources and associated mechanisms that
are capable of driving significant seismic activity, but to date no measurements of their …

The motion of a layered seabed induced by propagating gravity water waves is modelled by
the coupling matrix for a massless incompressible elastic bed according to Yamamoto. An …

The propagation of seismic interface waves is investigated in soft marine sediments in which
the density is constant, the shear modulus is small, and the profile of shear speed cs versus …

Low‐frequency sound propagation in shallow water environments is not restricted to the
water column but also involves the subbottom. Thus, as well as being important for …

As surface gravity water waves propagate through intermediate to shallow water, they
induce small motions of the seabed sediments through variations in hydro-dynamic pressure …

Direct measurement of the sediment shear-wave quality factor, Q β, has been hindered by
the lack of an effective shear-wave source. We show that if a satisfactory horizontal …

We use a combination of body wave and interface wave observations from an on‐bottom
seismic refraction survey to constrain the fine‐scale seismic structure of the upper crust in …