Finer grids in global climate models could lead to an improvement in the simulation of precipitat...
A multimodel, multiresolution set of simulations over the period 1950–2014 using a common forcing...
For seismic hazard assessment and earthquake hypocentre localization, detailed shear-wave velocit...
The Arctic region is projected to experience amplified warming as well as strongly increasing pre...
This study explores intra‐annual oscillations (IAOs) in upper thermospheric winds using GOCE cros...
The lower-thermosphere–ionosphere (LTI) system consists of the upper atmosphere and the lower par...
Although the knowledge of the gravity of the Earth has improved considerably with CHAMP, GRACE, a...
The Daedalus mission has been proposed to the European Space Agency (ESA) in response to the call...
Human activity causes vibrations that propagate into the ground as high-frequency seismic waves. ...
The perception of airborne infrasound (sounds below 20 Hz, inaudible to humans except at very hig...
After the launch of the Sentinel-5 Precursor satellite on 13 October 2017, its single payload, th...
Since 1991, induced earthquakes have been observed and linked to gas production in the Groningen ...
Recent developments in the densification of the seismic network covering the Groningen gas field ...
The continuous recordings of broadband seismometers on Saba and St. Eustatius in the Lesser Antil...
The detection and characterization of signals of interest in the presence of (in)coherent ambient...
In seismology and ocean acoustics, the interface with the atmosphere is typically represented as ...
Before the launch of the TROPOspheric Moni- toring Instrument (TROPOMI), only two other satellite...
The Tropospheric Monitoring Instrument (TROPOMI), aboard the Sentinel-5 Precursor (S5P) satellite...
It is important to understand how future environmental policies will impact both climate change a...