The record of seismic, hydroacoustic, and infrasonic waves is essential to detect, identify,
and localize sources of both natural and anthropogenic origin. To guarantee traceability and …

SUMMARY Between 0.1 and 0.5 Hz, infrasound signals recorded in the atmosphere are
dominated by ocean-generated noise called microbaroms. Microbaroms propagate through …

In the days following the January 12, 2010 M w 7 Haiti earthquake the shaking intensity near
the epicenter was overestimated and the spatial extent of the potentially damaging shaking …

The International Monitoring System (IMS) has been established since the late 1990s for the
verification of the Comprehensive Nuclear-Test-Ban Treaty (CTBT). The IMS is supposed to …

The receiver-to-source backazimuth of atmospheric infrasound signals is biased when cross-
winds are present along the propagation path. Infrasound from 598 surface explosions from …

Ground-based remote sensing of atmospheric parameters is often limited to single station
observations by vertical profiles at a certain geographic location. This is a limiting factor for …

The ionosphere represents part of the upper atmosphere. Its variability is observed on a
wide-scale temporal range from minutes, or even shorter, up to scales of the solar cycle and …

To facilitate infrasound propagation studies, we present AVO-G2S, an open-source, Ground-
to-Space model which provides temperature and wind specifications from the surface to an …

This study uses low‐frequency, inaudible acoustic waves (infrasound) to probe wind and
temperature fluctuations associated with breaking gravity waves (GWs) in the middle …

Detailed meteorological analyses based on observations extending through the middle
atmosphere (∼ 15 to 100 km altitude) can provide key information to whole atmosphere …