Long-term gravity field changes in Greenland and Antarctica from SLR data

In recent years, monitoring of changes in the Earth’s gravity field has been carried out mainly by the Gravity Recovery And Climate Experiment (GRACE) and its successor GRACE Follow-On. However, very little information is available on the temporal evolution of the Earth's gravity field prior to...

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Main Authors: Gałdyn, F., Sośnica, K., Zajdel, R., Meyer, U., Jäggi, A.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017838
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017838 2023-10-29T02:32:26+01:00 Long-term gravity field changes in Greenland and Antarctica from SLR data Gałdyn, F. Sośnica, K. Zajdel, R. Meyer, U. Jäggi, A. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017838 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1753 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017838 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1753 2023-10-01T23:43:19Z In recent years, monitoring of changes in the Earth’s gravity field has been carried out mainly by the Gravity Recovery And Climate Experiment (GRACE) and its successor GRACE Follow-On. However, very little information is available on the temporal evolution of the Earth's gravity field prior to the launch of the GRACE mission and through gaps in GRACE K-band data between 2010 and 2019. Fortunately, GRACE and GRACE Follow-On are not the only missions for the Earth's gravity field recovery. For the mass redistribution characteristics in large scales, we may employ Satellite Laser Ranging (SLR) observations to geodetic satellites. In this study, we derive gravity field changes for Greenland and Antarctica based on SLR data and compare the results to the GRACE, GRACE Follow-On, and Ice sheet Mass Balance Inter-comparison Exercise (IMBIE) data. We propose a set of long-term, continuous solutions, in which the gravity field is expanded up to degree and order 10/10 with a monthly resolution from 1/1995 to 10/2021. We show results from the unconstrained solution, as well as the solution that has been decomposed into normal equations expanded up to degree and order 4, 6, 8, and 10 and stacked, taking advantage of stability and better resolution from lowest and higher-degree expansion. We also propose different types of weighting, degree and order-specific constraining, and different data lengths. The SLR-based solutions are evaluated based on the noise on the oceans and differences to IMBIE and GRACE results for Greenland and Antarctica, which are identified by substantial ice mass loss. Conference Object Antarc* Antarctica Greenland Ice Sheet GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description In recent years, monitoring of changes in the Earth’s gravity field has been carried out mainly by the Gravity Recovery And Climate Experiment (GRACE) and its successor GRACE Follow-On. However, very little information is available on the temporal evolution of the Earth's gravity field prior to the launch of the GRACE mission and through gaps in GRACE K-band data between 2010 and 2019. Fortunately, GRACE and GRACE Follow-On are not the only missions for the Earth's gravity field recovery. For the mass redistribution characteristics in large scales, we may employ Satellite Laser Ranging (SLR) observations to geodetic satellites. In this study, we derive gravity field changes for Greenland and Antarctica based on SLR data and compare the results to the GRACE, GRACE Follow-On, and Ice sheet Mass Balance Inter-comparison Exercise (IMBIE) data. We propose a set of long-term, continuous solutions, in which the gravity field is expanded up to degree and order 10/10 with a monthly resolution from 1/1995 to 10/2021. We show results from the unconstrained solution, as well as the solution that has been decomposed into normal equations expanded up to degree and order 4, 6, 8, and 10 and stacked, taking advantage of stability and better resolution from lowest and higher-degree expansion. We also propose different types of weighting, degree and order-specific constraining, and different data lengths. The SLR-based solutions are evaluated based on the noise on the oceans and differences to IMBIE and GRACE results for Greenland and Antarctica, which are identified by substantial ice mass loss.
format Conference Object
author Gałdyn, F.
Sośnica, K.
Zajdel, R.
Meyer, U.
Jäggi, A.
spellingShingle Gałdyn, F.
Sośnica, K.
Zajdel, R.
Meyer, U.
Jäggi, A.
Long-term gravity field changes in Greenland and Antarctica from SLR data
author_facet Gałdyn, F.
Sośnica, K.
Zajdel, R.
Meyer, U.
Jäggi, A.
author_sort Gałdyn, F.
title Long-term gravity field changes in Greenland and Antarctica from SLR data
title_short Long-term gravity field changes in Greenland and Antarctica from SLR data
title_full Long-term gravity field changes in Greenland and Antarctica from SLR data
title_fullStr Long-term gravity field changes in Greenland and Antarctica from SLR data
title_full_unstemmed Long-term gravity field changes in Greenland and Antarctica from SLR data
title_sort long-term gravity field changes in greenland and antarctica from slr data
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017838
genre Antarc*
Antarctica
Greenland
Ice Sheet
genre_facet Antarc*
Antarctica
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/IUGG23-1753
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017838
op_doi https://doi.org/10.57757/IUGG23-1753
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