Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information

In this study the feasibility and performance of time variable decorrelation (VADER) filters derived from covariance information on decadal Gravity Recovery and Climate Experiment (GRACE) time series are investigated. The VADER filter is based on publicly available data that are provided by several...

Full description

Bibliographic Details
Published in:Geosciences
Main Authors: Alexander Horvath, Michael Murböck, Roland Pail, Martin Horwath
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2018
Subjects:
Online Access:https://doi.org/10.3390/geosciences8090323
https://doaj.org/article/daa3d0d78602468aa27cb627f5a790e8
id ftdoajarticles:oai:doaj.org/article:daa3d0d78602468aa27cb627f5a790e8
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:daa3d0d78602468aa27cb627f5a790e8 2023-05-15T14:02:15+02:00 Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information Alexander Horvath Michael Murböck Roland Pail Martin Horwath 2018-08-01T00:00:00Z https://doi.org/10.3390/geosciences8090323 https://doaj.org/article/daa3d0d78602468aa27cb627f5a790e8 EN eng MDPI AG http://www.mdpi.com/2076-3263/8/9/323 https://doaj.org/toc/2076-3263 2076-3263 doi:10.3390/geosciences8090323 https://doaj.org/article/daa3d0d78602468aa27cb627f5a790e8 Geosciences, Vol 8, Iss 9, p 323 (2018) GRACE gravity decorrelation filter post-processing Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.3390/geosciences8090323 2022-12-31T12:23:13Z In this study the feasibility and performance of time variable decorrelation (VADER) filters derived from covariance information on decadal Gravity Recovery and Climate Experiment (GRACE) time series are investigated. The VADER filter is based on publicly available data that are provided by several GRACE processing centers, and does not need its own Level-2 processing chain. Numerical closed loop simulations, incorporating stochastic and deterministic error budgets, serve as basis for the design of the filter setup, and the resulting filters are subsequently applied for real data processing. The closed loop experiments demonstrate the impact of temporally varying error and signal covariance matrices that are used for the design of decorrelation filters. The results indicate an average reduction of cumulative geoid height errors of 15% using time-variable instead of static decorrelation. Based on the simulation experience, a real data filtering procedure is designed and set up. It is applied to the ITSG-Grace2014 time variable gravity field time series with its associated full monthly covariance matrices. To assess the validity of the approach, linear mass trend estimates for the Antarctic Peninsula are computed using VADER filters and compared to previous estimates from both, GRACE and other mass balance estimation techniques. The mass change results obtained show very good agreement with other estimates and are robust against variations of the filter strength. The DDK decorrelation filter serves as main benchmark for the assessment of the VADER filter. For comparable filter strengths the VADER filters achieve a better de-striping and deliver smaller formal errors than static filters like the DDK. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Antarctic Peninsula Geosciences 8 9 323
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic GRACE
gravity
decorrelation
filter
post-processing
Geology
QE1-996.5
spellingShingle GRACE
gravity
decorrelation
filter
post-processing
Geology
QE1-996.5
Alexander Horvath
Michael Murböck
Roland Pail
Martin Horwath
Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
topic_facet GRACE
gravity
decorrelation
filter
post-processing
Geology
QE1-996.5
description In this study the feasibility and performance of time variable decorrelation (VADER) filters derived from covariance information on decadal Gravity Recovery and Climate Experiment (GRACE) time series are investigated. The VADER filter is based on publicly available data that are provided by several GRACE processing centers, and does not need its own Level-2 processing chain. Numerical closed loop simulations, incorporating stochastic and deterministic error budgets, serve as basis for the design of the filter setup, and the resulting filters are subsequently applied for real data processing. The closed loop experiments demonstrate the impact of temporally varying error and signal covariance matrices that are used for the design of decorrelation filters. The results indicate an average reduction of cumulative geoid height errors of 15% using time-variable instead of static decorrelation. Based on the simulation experience, a real data filtering procedure is designed and set up. It is applied to the ITSG-Grace2014 time variable gravity field time series with its associated full monthly covariance matrices. To assess the validity of the approach, linear mass trend estimates for the Antarctic Peninsula are computed using VADER filters and compared to previous estimates from both, GRACE and other mass balance estimation techniques. The mass change results obtained show very good agreement with other estimates and are robust against variations of the filter strength. The DDK decorrelation filter serves as main benchmark for the assessment of the VADER filter. For comparable filter strengths the VADER filters achieve a better de-striping and deliver smaller formal errors than static filters like the DDK.
format Article in Journal/Newspaper
author Alexander Horvath
Michael Murböck
Roland Pail
Martin Horwath
author_facet Alexander Horvath
Michael Murböck
Roland Pail
Martin Horwath
author_sort Alexander Horvath
title Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
title_short Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
title_full Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
title_fullStr Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
title_full_unstemmed Decorrelation of GRACE Time Variable Gravity Field Solutions Using Full Covariance Information
title_sort decorrelation of grace time variable gravity field solutions using full covariance information
publisher MDPI AG
publishDate 2018
url https://doi.org/10.3390/geosciences8090323
https://doaj.org/article/daa3d0d78602468aa27cb627f5a790e8
geographic Antarctic
The Antarctic
Antarctic Peninsula
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
genre_facet Antarc*
Antarctic
Antarctic Peninsula
op_source Geosciences, Vol 8, Iss 9, p 323 (2018)
op_relation http://www.mdpi.com/2076-3263/8/9/323
https://doaj.org/toc/2076-3263
2076-3263
doi:10.3390/geosciences8090323
https://doaj.org/article/daa3d0d78602468aa27cb627f5a790e8
op_doi https://doi.org/10.3390/geosciences8090323
container_title Geosciences
container_volume 8
container_issue 9
container_start_page 323
_version_ 1766272412109766656