Remote Sensing by Satellite Gravimetry

Over the last two decades, satellite gravimetry has become a new remote sensing technique that provides a detailed global picture of the physical structure of the Earth. With the CHAMP, GRACE, GOCE and GRACE Follow-On missions, mass distribution and mass transport in the Earth system can be systemat...

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Year of Publication:2021
Language:English
Physical Description:1 electronic resource (286 p.)
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520 |a Over the last two decades, satellite gravimetry has become a new remote sensing technique that provides a detailed global picture of the physical structure of the Earth. With the CHAMP, GRACE, GOCE and GRACE Follow-On missions, mass distribution and mass transport in the Earth system can be systematically observed and monitored from space. A wide range of Earth science disciplines benefit from these data, enabling improvements in applied models, providing new insights into Earth system processes (e.g., monitoring the global water cycle, ice sheet and glacier melting or sea-level rise) or establishing new operational services. Long time series of mass transport data are needed to disentangle anthropogenic and natural sources of climate change impacts on the Earth system. In order to secure sustained observations on a long-term basis, space agencies and the Earth science community are currently planning future satellite gravimetry mission concepts to enable higher accuracy and better spatial and temporal resolution. This Special Issue provides examples of recent improvements in gravity observation techniques and data processing and analysis, applications in the fields of hydrology, glaciology and solid Earth based on satellite gravimetry data, as well as concepts of future satellite constellations for monitoring mass transport in the Earth system. 
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653 |a terrestrial water storage (TWS) 
653 |a GRACE 
653 |a GLDAS 
653 |a TRMM 
653 |a drought 
653 |a ENSO 
653 |a NAO 
653 |a Turkey 
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653 |a Ice Sheets 
653 |a Sea-level Rise 
653 |a Antarctica 
653 |a CryoSat-2 
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653 |a GRACE-FO 
653 |a downward continuation 
653 |a spectral methods 
653 |a gravity field recovery 
653 |a GRACE Follow-On 
653 |a orbit configuration 
653 |a synergistic observation 
653 |a mass transport in the Earth system 
653 |a GRACE and GRACE follow-on mission 
653 |a current and future observation concepts and instruments 
653 |a GRACE TWSA 
653 |a groundwater level anomaly 
653 |a downscaling 
653 |a machine learning 
653 |a boosted regression trees 
653 |a glacial sediment 
653 |a ice mass 
653 |a satellite gravimetry 
653 |a Patagonia 
653 |a ice mass change 
653 |a SLR 
653 |a swarm 
653 |a normal equation combination 
653 |a coseismic gravity gradient changes 
653 |a gravity field model 
653 |a GOCE 
653 |a Earth’s gravity field 
653 |a kinematic orbit 
653 |a kinematic baseline 
653 |a time-variable gravity 
653 |a geocenter 
653 |a reference frames 
653 |a self-attraction and loading 
653 |a Level-2 processing 
653 |a time-variable gravity field 
653 |a mass change monitoring 
653 |a next-generation gravity mission 
653 |a temporal gravity field 
653 |a numerical closed-loop simulation 
653 |a satellite mission constellations 
653 |a mass transport 
653 |a gravity field satellite missions 
653 |a GOCE High-Level Processing Facility (HPF), earth gravity field 
653 |a geoid 
653 |a spectral enhancement method (SEM), GPS/leveling 
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