Global seismographic networks (GSNs) emerged during the late nineteenth and early
twentieth centuries, facilitated by seminal international developments in theory, technology …

In a context of global change and increasing anthropic pressure on the environment,
monitoring the Earth system and its evolution has become one of the key missions of …

We present a new approach to characterize the background seismic noise across the
continental United States. Using this approach, power spectral density (PSD) is estimated at …

The aim of this paper is to discuss the existing scientific literature in order to gather all the
available information dealing with the origin and the nature of the ambient seismic noise …

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 …

Analysis of continuous seismic data recorded by a dense passive seismological network (Hi‐
CLIMB) installed across the Himalayas reveals strong spatial and temporal variations in the …

In the absence of earthquakes, oceanic microseisms are the strongest signals recorded by
seismic stations. Using the GEOSCOPE global seismic network, we show that the secondary …

This article describes a new method to estimate (1) the self-noise as a function of frequency
of three-channel, linear systems and (2) the relative transfer functions between the channels …

The Seismic Wavefield provides a guide to the understanding of seismograms in terms of
physical propagation processes within the Earth. The focus is on the observation of …

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 …