High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP

This progress report summarizes the research work conducted under NASA's Solid Earth and Natural Hazards Program 1998 (SENH98) entitled High Resolution Gravity and Time Varying Gravity Field Recovery Using GRACE (Gravity Recovery and Climate Experiment) and CHAMP (Challenging Mini-satellite Pac...

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Main Author: Shum, C. K.
Language:unknown
Published: 2002
Subjects:
Online Access:http://hdl.handle.net/2060/20030014727
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20030014727 2023-05-15T16:41:17+02:00 High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP Shum, C. K. Unclassified, Unlimited, Publicly available Dec. 20, 2002 application/pdf http://hdl.handle.net/2060/20030014727 unknown Document ID: 20030014727 http://hdl.handle.net/2060/20030014727 No Copyright CASI Space Processing 2002 ftnasantrs 2019-07-21T02:29:30Z This progress report summarizes the research work conducted under NASA's Solid Earth and Natural Hazards Program 1998 (SENH98) entitled High Resolution Gravity and Time Varying Gravity Field Recovery Using GRACE (Gravity Recovery and Climate Experiment) and CHAMP (Challenging Mini-satellite Package for Geophysical Research and Applications), which included a no-cost extension time period. The investigation has conducted pilot studies to use the simulated GRACE and CHAMP data and other in situ and space geodetic observable, satellite altimeter data, and ocean mass variation data to study the dynamic processes of the Earth which affect climate change. Results from this investigation include: (1) a new method to use the energy approach for expressing gravity mission data as in situ measurements with the possibility to enhance the spatial resolution of the gravity signal; (2) the method was tested using CHAMP and validated with the development of a mean gravity field model using CHAMP data, (3) elaborate simulation to quantify errors of tides and atmosphere and to recover hydrological and oceanic signals using GRACE, results show that there are significant aliasing effect and errors being amplified in the GRACE resonant geopotential and it is not trivial to remove these errors, and (4) quantification of oceanic and ice sheet mass changes in a geophysical constraint study to assess their contributions to global sea level change, while the results improved significant over the use of previous studies using only the SLR (Satellite Laser Ranging)-determined zonal gravity change data, the constraint could be further improved with additional information on mantle rheology, PGR (Post-Glacial Rebound) and ice loading history. A list of relevant presentations and publications is attached, along with a summary of the SENH investigation generated in 2000. Other/Unknown Material Ice Sheet NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Space Processing
spellingShingle Space Processing
Shum, C. K.
High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
topic_facet Space Processing
description This progress report summarizes the research work conducted under NASA's Solid Earth and Natural Hazards Program 1998 (SENH98) entitled High Resolution Gravity and Time Varying Gravity Field Recovery Using GRACE (Gravity Recovery and Climate Experiment) and CHAMP (Challenging Mini-satellite Package for Geophysical Research and Applications), which included a no-cost extension time period. The investigation has conducted pilot studies to use the simulated GRACE and CHAMP data and other in situ and space geodetic observable, satellite altimeter data, and ocean mass variation data to study the dynamic processes of the Earth which affect climate change. Results from this investigation include: (1) a new method to use the energy approach for expressing gravity mission data as in situ measurements with the possibility to enhance the spatial resolution of the gravity signal; (2) the method was tested using CHAMP and validated with the development of a mean gravity field model using CHAMP data, (3) elaborate simulation to quantify errors of tides and atmosphere and to recover hydrological and oceanic signals using GRACE, results show that there are significant aliasing effect and errors being amplified in the GRACE resonant geopotential and it is not trivial to remove these errors, and (4) quantification of oceanic and ice sheet mass changes in a geophysical constraint study to assess their contributions to global sea level change, while the results improved significant over the use of previous studies using only the SLR (Satellite Laser Ranging)-determined zonal gravity change data, the constraint could be further improved with additional information on mantle rheology, PGR (Post-Glacial Rebound) and ice loading history. A list of relevant presentations and publications is attached, along with a summary of the SENH investigation generated in 2000.
author Shum, C. K.
author_facet Shum, C. K.
author_sort Shum, C. K.
title High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
title_short High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
title_full High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
title_fullStr High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
title_full_unstemmed High-Resolution Gravity and Time-Varying Gravity Field Recovery using GRACE and CHAMP
title_sort high-resolution gravity and time-varying gravity field recovery using grace and champ
publishDate 2002
url http://hdl.handle.net/2060/20030014727
op_coverage Unclassified, Unlimited, Publicly available
genre Ice Sheet
genre_facet Ice Sheet
op_source CASI
op_relation Document ID: 20030014727
http://hdl.handle.net/2060/20030014727
op_rights No Copyright
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