Javascript must be enabled to continue!
tatistically optimal Slepian method for processing GRACE Level 2 data
View through CrossRef
The global surface mass variations obtained by the Gravity Recovery and Climate Experiment (GRACE) satellite Level-2 products show significant north-south strip noise, which seriously affects the estimation of regional surface mass variations. Most existing filtering methods are based on the processing of spherical harmonic basis functions to remove stripes. However, because spherical harmonic basis functions are only orthogonal globally, they may not be orthogonal in regions, which hinders the effective constraint of quality changes in specific regions. Therefore, this paper converts the spherical harmonic base of GRACE Level-2 to the Slepian base of the interested region and truncates it based on the Shannon number of the region. Even though the signals are concentrated in the region, there are still many stripes present. In order to remove the stripes, it is necessary to introduce the regularization and consider the statistical information of the spherical harmonic coefficient. The Tikhonov regularization matrix of the Slepian coefficient is obtained, combined with a power-law model to construct the prior covariance matrix of the signal and the optimal regularization coefficient is selected by using the generalized cross-validation (GCV) method, which is represented as the statistically optimal Slepian method (SO-Slepian) in this study. The results show that the ability of SO-Slepian and decorrelation and denoising kernel (DDK) filtering with the same regularization parameters as SO-Slepian to remove stripes and retain signals in the selected region is comparable. The line chart comparing the differences between SO-Slepian and DDK not only demonstrates the close similarity in results between SO-Slepian and traditional DDK filtering in the regional domain but also emphasizes the logical application of regularization during the Slepian modeling stage. It further supports the rationality of developing a regularization scheme for GRACE data processing based on Slepian.
Institute of Rock Structure and Mechanics, AS CR
Title: tatistically optimal Slepian method for processing GRACE Level 2 data
Description:
The global surface mass variations obtained by the Gravity Recovery and Climate Experiment (GRACE) satellite Level-2 products show significant north-south strip noise, which seriously affects the estimation of regional surface mass variations.
Most existing filtering methods are based on the processing of spherical harmonic basis functions to remove stripes.
However, because spherical harmonic basis functions are only orthogonal globally, they may not be orthogonal in regions, which hinders the effective constraint of quality changes in specific regions.
Therefore, this paper converts the spherical harmonic base of GRACE Level-2 to the Slepian base of the interested region and truncates it based on the Shannon number of the region.
Even though the signals are concentrated in the region, there are still many stripes present.
In order to remove the stripes, it is necessary to introduce the regularization and consider the statistical information of the spherical harmonic coefficient.
The Tikhonov regularization matrix of the Slepian coefficient is obtained, combined with a power-law model to construct the prior covariance matrix of the signal and the optimal regularization coefficient is selected by using the generalized cross-validation (GCV) method, which is represented as the statistically optimal Slepian method (SO-Slepian) in this study.
The results show that the ability of SO-Slepian and decorrelation and denoising kernel (DDK) filtering with the same regularization parameters as SO-Slepian to remove stripes and retain signals in the selected region is comparable.
The line chart comparing the differences between SO-Slepian and DDK not only demonstrates the close similarity in results between SO-Slepian and traditional DDK filtering in the regional domain but also emphasizes the logical application of regularization during the Slepian modeling stage.
It further supports the rationality of developing a regularization scheme for GRACE data processing based on Slepian.
Related Results
The research unit NEROGRAV: first results on stochastic modeling for gravity field determination with real GRACE and GRACE-FO data
The research unit NEROGRAV: first results on stochastic modeling for gravity field determination with real GRACE and GRACE-FO data
<p>The central hypothesis of the Research Unit (RU) NEROGRAV (New Refined Observations of Climate Change from Spaceborne Gravity Missions), funded for three years by ...
Assessing Detectability of Global Flood Occurrences using Daily and Monthly GRACE/GRACE-FO
Assessing Detectability of Global Flood Occurrences using Daily and Monthly GRACE/GRACE-FO
<p>&#160;</p>
<p>Floods pose a threat to the lives of millions of people globally each year, with economic losses exceeding those ...
Impact of Admission Serum Calcium Level Added on Grace Risk Score for Predicting In-Hospital Adverse Outcome in Patients with Acute Coronary Syndrome
Impact of Admission Serum Calcium Level Added on Grace Risk Score for Predicting In-Hospital Adverse Outcome in Patients with Acute Coronary Syndrome
Background: Abnormal calcium metabolism predicts worse outcomes after acute coronary syndrome (ACS). However, this parameter is not included in risk prediction scores, including GR...
Revisiting excitation of length-of-day using recent GRACE/GRACE-FO, SLR, SLR+GRACE/GRACE-FO gravity solutions and geophysical models
Revisiting excitation of length-of-day using recent GRACE/GRACE-FO, SLR, SLR+GRACE/GRACE-FO gravity solutions and geophysical models
Variations in Earth’s rotation, encompassing polar motion (PM) and the length-of-day (LOD) changes, result from a variety of factors influencing mass distribution and mov...
Combined Gravity Solution from SLR and GRACE/GRACE-FO
Combined Gravity Solution from SLR and GRACE/GRACE-FO
Abstract
The recovery of Earth’s time variable gravity field from satellite data relied heavily on Satellite Laser Ranging (SLR) before the recent GRACE and GRACE Follow-...
Towards 30-years of mass change observations: GRACE Follow-On extended mission phase, and GRACE-Continuity developments 
Towards 30-years of mass change observations: GRACE Follow-On extended mission phase, and GRACE-Continuity developments 
The GRACE Follow-On (GRACE-FO) satellite mission, a partnership between NASA (US) and GFZ (Germany), successfully completed its nominal five-year prime mission phase in May 2023, a...
A traceable GRACE/GRACE-FO Level-1C scientific dataset (2002-2026) for reproducible mass-change analysis
A traceable GRACE/GRACE-FO Level-1C scientific dataset (2002-2026) for reproducible mass-change analysis
While monthly Level-2 products of GRACE/-FO are widely used as essential climate variables for mass-transport studies, published processing chains and intermediate outputs are ofte...
Martin Luther on Grace
Martin Luther on Grace
Abstract
Grace is an essential element of Christian theological reflection. Primarily, the divine attribute or trait labeled “grace” refers to God’s disposition a...

