Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations

We present a state-of-the-art approach of passive-ocean Modified Radial Basis Functions (MRBFs) that improves the recovery of time-variable gravity fields from GRACE. As is well known, spherical harmonics (SHs), which are commonly used to recover gravity fields, are orthogonal basis functions with g...

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Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Yang, Fan, Kusche, Jürgen, Forootan, Ehsan, Rietbroek, Roelof
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2017
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/103115/
https://doi.org/10.1002/2016JB013633
https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf
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spelling ftunivcardiff:oai:https://orca.cardiff.ac.uk:103115 2023-05-15T16:29:54+02:00 Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations Yang, Fan Kusche, Jürgen Forootan, Ehsan Rietbroek, Roelof 2017-08-01 application/pdf https://orca.cardiff.ac.uk/id/eprint/103115/ https://doi.org/10.1002/2016JB013633 https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf en eng Wiley-Blackwell https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf Yang, Fan, Kusche, Jürgen, Forootan, Ehsan https://orca.cardiff.ac.uk/view/cardiffauthors/A2261102I.html orcid:0000-0003-3055-041X orcid:0000-0003-3055-041X and Rietbroek, Roelof 2017. Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations. Journal of Geophysical Research: Solid Earth 122 (8) , pp. 6875-6892. 10.1002/2016JB013633 https://doi.org/10.1002/2016JB013633 file https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf doi:10.1002/2016JB013633 Article PeerReviewed 2017 ftunivcardiff https://doi.org/10.1002/2016JB013633 2022-11-03T23:42:51Z We present a state-of-the-art approach of passive-ocean Modified Radial Basis Functions (MRBFs) that improves the recovery of time-variable gravity fields from GRACE. As is well known, spherical harmonics (SHs), which are commonly used to recover gravity fields, are orthogonal basis functions with global coverage. However, the chosen SH truncation involves a global compromise between data coverage and obtainable resolution, and strong localized signals may not be fully captured. Radial basis functions (RBFs) provide another representation, which has been proposed in earlier works to be better suited to retrieve regional gravity signals. In this paper, we propose a MRBF approach by embedding the known coastal geometries in the RBF parameterization and imposing global mass conservation and equilibrium behavior of the oceans. Our hypothesis is that, with this physically justified constraint, the GRACE-derived gravity signals can be more realistically partitioned into the land and ocean contributions along the coastlines. We test this new technique to invert monthly gravity fields from GRACE level-1b observations covering 2005-2010, for which the numerical results indicate that: (1) MRBF-based solutions reduce the number of parameters by approximately 10%, and allow for more flexible regularization when compared to ordinary RBF solutions; and (2) the MRBF-derived mass flux is better confined along coastal areas. The latter is particularly tested in the Southern Greenland, and our results indicate that the trend of mass loss from the MRBF solutions is approximately 11% larger than that from the SH solutions, and approximately 4% ∼ 6% larger than that of RBF solutions. Article in Journal/Newspaper Greenland Cardiff University: ORCA (Online Research @ Cardiff) Greenland Journal of Geophysical Research: Solid Earth 122 8 6875 6892
institution Open Polar
collection Cardiff University: ORCA (Online Research @ Cardiff)
op_collection_id ftunivcardiff
language English
description We present a state-of-the-art approach of passive-ocean Modified Radial Basis Functions (MRBFs) that improves the recovery of time-variable gravity fields from GRACE. As is well known, spherical harmonics (SHs), which are commonly used to recover gravity fields, are orthogonal basis functions with global coverage. However, the chosen SH truncation involves a global compromise between data coverage and obtainable resolution, and strong localized signals may not be fully captured. Radial basis functions (RBFs) provide another representation, which has been proposed in earlier works to be better suited to retrieve regional gravity signals. In this paper, we propose a MRBF approach by embedding the known coastal geometries in the RBF parameterization and imposing global mass conservation and equilibrium behavior of the oceans. Our hypothesis is that, with this physically justified constraint, the GRACE-derived gravity signals can be more realistically partitioned into the land and ocean contributions along the coastlines. We test this new technique to invert monthly gravity fields from GRACE level-1b observations covering 2005-2010, for which the numerical results indicate that: (1) MRBF-based solutions reduce the number of parameters by approximately 10%, and allow for more flexible regularization when compared to ordinary RBF solutions; and (2) the MRBF-derived mass flux is better confined along coastal areas. The latter is particularly tested in the Southern Greenland, and our results indicate that the trend of mass loss from the MRBF solutions is approximately 11% larger than that from the SH solutions, and approximately 4% ∼ 6% larger than that of RBF solutions.
format Article in Journal/Newspaper
author Yang, Fan
Kusche, Jürgen
Forootan, Ehsan
Rietbroek, Roelof
spellingShingle Yang, Fan
Kusche, Jürgen
Forootan, Ehsan
Rietbroek, Roelof
Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
author_facet Yang, Fan
Kusche, Jürgen
Forootan, Ehsan
Rietbroek, Roelof
author_sort Yang, Fan
title Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
title_short Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
title_full Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
title_fullStr Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
title_full_unstemmed Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations
title_sort passive-ocean radial basis function approach to improve temporal gravity recovery from grace observations
publisher Wiley-Blackwell
publishDate 2017
url https://orca.cardiff.ac.uk/id/eprint/103115/
https://doi.org/10.1002/2016JB013633
https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_relation https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf
Yang, Fan, Kusche, Jürgen, Forootan, Ehsan https://orca.cardiff.ac.uk/view/cardiffauthors/A2261102I.html orcid:0000-0003-3055-041X orcid:0000-0003-3055-041X and Rietbroek, Roelof 2017. Passive-ocean radial basis function approach to improve temporal gravity recovery from GRACE observations. Journal of Geophysical Research: Solid Earth 122 (8) , pp. 6875-6892. 10.1002/2016JB013633 https://doi.org/10.1002/2016JB013633 file https://orca.cardiff.ac.uk/id/eprint/103115/1/YangForootan_JGR2017.pdf
doi:10.1002/2016JB013633
op_doi https://doi.org/10.1002/2016JB013633
container_title Journal of Geophysical Research: Solid Earth
container_volume 122
container_issue 8
container_start_page 6875
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