The last decade witnessed an explosion in yearly number of publications on passive glacier
seismology. The seismic signals from a wide range of glacier‐related processes fill a broad …

Two thirds of the surface of our planet are covered by water and are still poorly instrumented,
which has prevented the earth science community from addressing numerous key scientific …

Noise with periods 3 to 10 s, ubiquitous in seismic records, is expected to be mostly
generated by pairs of ocean wave trains of opposing propagation directions with half the …

Stacks of ambient noise cross-correlations are more and more routinely used to extract
empirical Green's functions between station pairs. The success of the cross-correlations is …

The increasing number of broad-band seismic stations recording the full spectrum of the
seismic wavefield continuously has boosted interest in background signals recorded in the …

The strongest seismic noise, called secondary microseisms, is generated by ocean wave
interactions and we model this noise using the theory of Longuet-Higgins generalized to …

Sea waves constitute a natural phenomenon with a great impact on human activities, and
their monitoring is essential for meteorology, coastal safety, navigation, and renewable …

Seismic noise recorded at the surface of Mars has been monitored since February 2019,
using the InSight seismometers. This noise can reach− 200 dB. It is 500 times lower than on …

This document presents a summary of the 2023 Terrestrial Very-Long-Baseline Atom
Interferometry Workshop hosted by CERN. The workshop brought together experts from …

We performed a frequency‐dependent polarization analysis on ambient seismic energy
recorded by 1768 USArray Transportable Array (TA) seismometers for the time period of 1 …