Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices

Satellite gravimetry as realized by the GRACE and GRACE-FO missions (both referred to as GRACE in the following) is a major observation for ice mass balance estimates. Thereby, GRACE-based studies were often conducted separately for either the Antarctic Ice Sheet, the Greenland Ice Sheet, or the glo...

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Main Authors: Döhne, T., Horwath, M., Tripathi, V.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021142
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021142 2023-07-30T03:59:15+02:00 Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices Döhne, T. Horwath, M. Tripathi, V. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021142 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4734 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021142 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4734 2023-07-09T23:40:20Z Satellite gravimetry as realized by the GRACE and GRACE-FO missions (both referred to as GRACE in the following) is a major observation for ice mass balance estimates. Thereby, GRACE-based studies were often conducted separately for either the Antarctic Ice Sheet, the Greenland Ice Sheet, or the global glacier domain or selected glacier regions. The start of the Glacier Mass Balance Intercomparison Exercise (GLAMBIE) in addition to the Ice-sheet Mass Balance Intercomparison Exercise (IMBIE) gives new impetus to questions about the consistency between GRACE-based estimates for different land ice domains and about the sensitivity of the estimates to methodological choices. We report investigations on a consistent land ice mass balance estimate based on our tailored sensitivity kernel approach previously applied to the Antarctic Ice Sheet and the Greenland Ice Sheet. In the tailored sensitivity kernel approach the sensitivity kernel of the mass change estimator is directly optimized in a formal minimization of propagated GRACE solution errors and leakage errors. The focus on specific regions is realized by 'tailoring' the method to the signal of interest based on available signal covariance information of mass changes, without violating global consistency of the analysis. We show via a sensitivity analysis how different parameters of the estimation method (such as weighting of GRACE error covariance information, degree of external information employed for the signal covariance information, and accounting for sea-level fingerprints) influence the resulting mass change estimates. Conference Object Antarc* Antarctic glacier Greenland Ice Sheet GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic Greenland The Antarctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Satellite gravimetry as realized by the GRACE and GRACE-FO missions (both referred to as GRACE in the following) is a major observation for ice mass balance estimates. Thereby, GRACE-based studies were often conducted separately for either the Antarctic Ice Sheet, the Greenland Ice Sheet, or the global glacier domain or selected glacier regions. The start of the Glacier Mass Balance Intercomparison Exercise (GLAMBIE) in addition to the Ice-sheet Mass Balance Intercomparison Exercise (IMBIE) gives new impetus to questions about the consistency between GRACE-based estimates for different land ice domains and about the sensitivity of the estimates to methodological choices. We report investigations on a consistent land ice mass balance estimate based on our tailored sensitivity kernel approach previously applied to the Antarctic Ice Sheet and the Greenland Ice Sheet. In the tailored sensitivity kernel approach the sensitivity kernel of the mass change estimator is directly optimized in a formal minimization of propagated GRACE solution errors and leakage errors. The focus on specific regions is realized by 'tailoring' the method to the signal of interest based on available signal covariance information of mass changes, without violating global consistency of the analysis. We show via a sensitivity analysis how different parameters of the estimation method (such as weighting of GRACE error covariance information, degree of external information employed for the signal covariance information, and accounting for sea-level fingerprints) influence the resulting mass change estimates.
format Conference Object
author Döhne, T.
Horwath, M.
Tripathi, V.
spellingShingle Döhne, T.
Horwath, M.
Tripathi, V.
Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
author_facet Döhne, T.
Horwath, M.
Tripathi, V.
author_sort Döhne, T.
title Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
title_short Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
title_full Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
title_fullStr Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
title_full_unstemmed Globally consistent land ice mass balance estimates from GRACE/GRACE-FO: Sensitivity to methodological choices
title_sort globally consistent land ice mass balance estimates from grace/grace-fo: sensitivity to methodological choices
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021142
geographic Antarctic
Greenland
The Antarctic
geographic_facet Antarctic
Greenland
The Antarctic
genre Antarc*
Antarctic
glacier
Greenland
Ice Sheet
genre_facet Antarc*
Antarctic
glacier
Greenland
Ice Sheet
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4734
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021142
op_doi https://doi.org/10.57757/IUGG23-4734
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