This review covers basic theory and techniques behind the use of ground-based gravimetry
at the Earth's surface. The orientation is toward modern instrumentation, data processing …

The Earth tides are the motions induced in the solid Earth, and the changes in its
gravitational potential, induced by the tidal forces from external bodies.(These forces, acting …

For observations of vertical‐component acceleration in the normal‐mode band (0.3–10
mHz), the detection sensitivity for signals from the Earth's body can be improved to levels …

Since the beginning of the Global Geodynamics Project (GGP) in 1997, the number of
superconducting gravimeters (SG s) has increased to reach 30 operating sites today. Data …

We report on the results of a comparative analysis carried out on more than ten months of co-
located records collected at the J9 gravity station in Strasbourg (France) with a new …

Abstract Since July 2015 a Superconducting Gravimeter (SG) of the latest generation, the
iOSG-24, has been recording continuously the time-varying gravity field at the low noise …

An approach for the evaluation of local hydrological modelling is presented: the deployment
of temporal terrestrial gravity measurements and gravimetric 3-D modelling in addition to …

The Mw> 9 Sumatra‐Andaman earthquake on December 26, 2004 has strongly excited the
low‐frequency seismic modes and is a unique opportunity to improve the frequency and …

Gravimetry is a well-established tool to probe the deep Earth's processes. Geophysical
signals coming from the deep Earth, like the inner core free oscillations, have however never …

Gravity recovery and climate experiment (GRACE)-derived temporal gravity variations can
be resolved within the μgal (10− 8 m/s 2) range, if we restrict the spatial resolution to a half …