FN Archimer Export Format
PT J
TI Applications and Challenges of GRACE and GRACE Follow-On Satellite Gravimetry
BT 
AF Chen, Jianli
   Cazenave, Anny
   Dahle, Christoph
   Llovel, William
   Panet, Isabelle
   Pfeffer, Julia
   Moreira, Lorena
AS 1:1;2:2,7;3:3;4:4;5:5;6:6;7:7;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Center for Space Research, University of Texas at Austin, Austin, TX, 78759, USA
   Legos/CNES, 14 Avenue Edouard Belin, 31400, Toulouse, France
   GFZ German Research Centre for Geosciences, 14473, Potsdam, Germany
   LOPS, University of Brest/IFREMER/IRD/CNRS, 29280, Brest, France
   Université de Paris, IPGP/CNRS/IGN, 75005, Paris, France
   Magellium, 31520, Ramonville Saint-Agne, France
   International Space Science Institute, Hallerstrasse 6, 3012, Bern, Switzerland
C2 UNIV TEXAS AUSTIN, USA
   CNES, FRANCE
   GFZ, GERMANY
   CNRS, FRANCE
   UNIV PARIS, FRANCE
   MAGELLIUM, FRANCE
   ISSI, SWITZERLAND
UM LOPS
IN WOS Cotutelle UMR
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
IF 4.6
TC 66
UR https://archimer.ifremer.fr/doc/00746/85814/90968.pdf
LA English
DT Article
DE ;GRACE;GRACE-FO;Satellite gravimetry;Gravity;Mass change;Application;Challenge
AB Time-variable gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) missions have opened up a new avenue of opportunities for studying large-scale mass redistribution and transport in the Earth system. Over the past 19 years, GRACE/GRACE-FO time-variable gravity measurements have been widely used to study mass variations in different components of the Earth system, including the hydrosphere, ocean, cryosphere, and solid Earth, and significantly improved our understanding of long-term variability of the climate system. We carry out a comprehensive review of GRACE/GRACE-FO satellite gravimetry, time-variable gravity fields, data processing methods, and major applications in several different fields, including terrestrial water storage change, global ocean mass variation, ice sheets and glaciers mass balance, and deformation of the solid Earth. We discuss in detail several major challenges we need to face when using GRACE/GRACE-FO time-variable gravity measurements to study mass changes, and how we should address them. We also discuss the potential of satellite gravimetry in detecting gravitational changes that are believed to originate from the deep Earth. The extended record of GRACE/GRACE-FO gravity series, with expected continuous improvements in the coming years, will lead to a broader range of applications and improve our understanding of both climate change and the Earth system. Article Highlights A comprehensive review of major applications of GRACE/GRACE-FO satellite gravimetry Discussions in detail of some major challenges in GRACE/GRACE-FO mass change estimation Discussions of the potential detection of deep Earth signals by GRACE/GRACE-FO gravimetry 
PY 2022
PD FEB
SO Surveys In Geophysics
SN 0169-3298
PU Springer Science and Business Media LLC
VL 43
IS 1
UT 000740405600001
BP 305
EP 345
DI 10.1007/s10712-021-09685-x
ID 85814
ER

EF