GRACE, time-varying gravity, Earth system dynamics and climate change
B Wouters, JA Bonin, DP Chambers… - Reports on Progress …, 2014 - iopscience.iop.org
Continuous observations of temporal variations in the Earth's gravity field have recently
become available at an unprecedented resolution of a few hundreds of kilometers. The …
become available at an unprecedented resolution of a few hundreds of kilometers. The …
Decorrelated GRACE time-variable gravity solutions by GFZ, and their validation using a hydrological model
J Kusche, R Schmidt, S Petrovic, R Rietbroek - Journal of geodesy, 2009 - Springer
We have analyzed recent gravity recovery and climate experiment (GRACE) RL04 monthly
gravity solutions, using a new decorrelating post-processing approach. We find very good …
gravity solutions, using a new decorrelating post-processing approach. We find very good …
GRACE Hydrological estimates for small basins: Evaluating processing approaches on the High Plains Aquifer, USA
L Longuevergne, BR Scanlon… - Water Resources …, 2010 - Wiley Online Library
The Gravity Recovery and Climate Experiment (GRACE) satellites provide observations of
water storage variation at regional scales. However, when focusing on a region of interest …
water storage variation at regional scales. However, when focusing on a region of interest …
The design of an optimal filter for monthly GRACE gravity models
Most applications of the publicly released Gravity Recovery and Climate Experiment monthly
gravity field models require the application of a spatial filter to help suppressing noise and …
gravity field models require the application of a spatial filter to help suppressing noise and …
Coseismic and postseismic deformation of the 2011 Tohoku‐Oki earthquake constrained by GRACE gravimetry
Spaceborne gravimetry data from the Gravity Recovery And Climate Experiment (GRACE)
are processed using spatio‐spectral Slepian localization analysis enabling the high …
are processed using spatio‐spectral Slepian localization analysis enabling the high …
Separation of coseismic and postseismic gravity changes for the 2004 Sumatra–Andaman earthquake from 4.6 yr of GRACE observations and modelling of the …
C De Linage, L Rivera, J Hinderer… - Geophysical Journal …, 2009 - academic.oup.com
This paper is devoted to the simultaneous determination of the coseismic and postseismic
gravitational changes caused by the great 2004 December 26 Sumatra–Andaman …
gravitational changes caused by the great 2004 December 26 Sumatra–Andaman …
Source parameter inversion for recent great earthquakes from a decade‐long observation of global gravity fields
We quantify gravity changes after great earthquakes present within the 10 year long time
series of monthly Gravity Recovery and Climate Experiment (GRACE) gravity fields. Using …
series of monthly Gravity Recovery and Climate Experiment (GRACE) gravity fields. Using …
Upper mantle rheology from GRACE and GPS postseismic deformation after the 2004 Sumatra‐Andaman earthquake
Mantle rheology is one of the essential, yet least understood, material properties of our
planet, controlling the dynamic processes inside the Earth's mantle and the Earth's response …
planet, controlling the dynamic processes inside the Earth's mantle and the Earth's response …
A new GRACE filtering approach based on iterative image convolution
H Zhou, P Wang, L Tang, Z Luo - Journal of Geophysical …, 2023 - Wiley Online Library
Abstract The Gravity Recovery and Climate Experiment (GRACE) mission and its successor
GRACE Follow‐On (GRACE‐FO) mission provide humans with a unique perspective on …
GRACE Follow‐On (GRACE‐FO) mission provide humans with a unique perspective on …
Implications of postseismic gravity change following the great 2004 Sumatra‐Andaman earthquake from the regional harmonic analysis of GRACE intersatellite …
We report Gravity Recovery and Climate Experiment (GRACE) satellite observations of
coseismic displacements and postseismic transients from the great Sumatra‐Andaman …
coseismic displacements and postseismic transients from the great Sumatra‐Andaman …