Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...

Time-variable gravity field models obtained from satellite gravimetric techniques allow for the assessment of ice sheet mass changes in remote polar regions, such as Greenland and Antarctica. So far, GRACE has been the primary mission for obtaining the global time-variable gravity field models. Howe...

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Main Authors: Gałdyn, Filip, Sośnica, Krzysztof, Zajdel, Radosław, Meyer, Ulrich, Jäggi, Adrian
Format: Article in Journal/Newspaper
Language:English
Published: OMEGA-PSIR 2024
Subjects:
Online Access:https://dx.doi.org/10.57755/xnaf-mv77
https://bazawiedzy.upwr.edu.pl/info/article/UPWR8eeb3a088ebd474695b68fcffdec7929/
id ftdatacite:10.57755/xnaf-mv77
record_format openpolar
spelling ftdatacite:10.57755/xnaf-mv77 2024-04-28T08:02:52+00:00 Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ... Gałdyn, Filip Sośnica, Krzysztof Zajdel, Radosław Meyer, Ulrich Jäggi, Adrian 2024 https://dx.doi.org/10.57755/xnaf-mv77 https://bazawiedzy.upwr.edu.pl/info/article/UPWR8eeb3a088ebd474695b68fcffdec7929/ en eng OMEGA-PSIR https://bazawiedzy.upwr.edu.pl/info/journalseries/WUT64574/ Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Ice mass balance, time-variable gravity field determination, GRACE, GRACE Follow-On, SLR, Earth’s, gravity models JournalArticle article-journal ScholarlyArticle 2024 ftdatacite https://doi.org/10.57755/xnaf-mv77 2024-04-02T11:20:25Z Time-variable gravity field models obtained from satellite gravimetric techniques allow for the assessment of ice sheet mass changes in remote polar regions, such as Greenland and Antarctica. So far, GRACE has been the primary mission for obtaining the global time-variable gravity field models. However, GRACE was launched in 2002, thus very little is known about the global mass changes before this data, as well as between GRACE and its successor – GRACE Follow-On. We derive a method of gravity field recovery based on Satellite Laser Ranging (SLR) data to geodetic satellites that allows for obtaining direct ice mass change estimates for a period longer by 10 years than that provided by the GRACE missions. The developed method is based on splitting normal equation systems and re-stacking the solutions which allow for stable inversion, reduces the correlations between obtained parameters, stabilizes the ice mass estimates in polar regions, and reduces the noise over oceans by a factor of four. The secular ... Article in Journal/Newspaper Antarc* Antarctica Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Ice mass balance, time-variable gravity field determination, GRACE, GRACE Follow-On, SLR, Earth’s, gravity models
spellingShingle Ice mass balance, time-variable gravity field determination, GRACE, GRACE Follow-On, SLR, Earth’s, gravity models
Gałdyn, Filip
Sośnica, Krzysztof
Zajdel, Radosław
Meyer, Ulrich
Jäggi, Adrian
Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
topic_facet Ice mass balance, time-variable gravity field determination, GRACE, GRACE Follow-On, SLR, Earth’s, gravity models
description Time-variable gravity field models obtained from satellite gravimetric techniques allow for the assessment of ice sheet mass changes in remote polar regions, such as Greenland and Antarctica. So far, GRACE has been the primary mission for obtaining the global time-variable gravity field models. However, GRACE was launched in 2002, thus very little is known about the global mass changes before this data, as well as between GRACE and its successor – GRACE Follow-On. We derive a method of gravity field recovery based on Satellite Laser Ranging (SLR) data to geodetic satellites that allows for obtaining direct ice mass change estimates for a period longer by 10 years than that provided by the GRACE missions. The developed method is based on splitting normal equation systems and re-stacking the solutions which allow for stable inversion, reduces the correlations between obtained parameters, stabilizes the ice mass estimates in polar regions, and reduces the noise over oceans by a factor of four. The secular ...
format Article in Journal/Newspaper
author Gałdyn, Filip
Sośnica, Krzysztof
Zajdel, Radosław
Meyer, Ulrich
Jäggi, Adrian
author_facet Gałdyn, Filip
Sośnica, Krzysztof
Zajdel, Radosław
Meyer, Ulrich
Jäggi, Adrian
author_sort Gałdyn, Filip
title Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
title_short Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
title_full Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
title_fullStr Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
title_full_unstemmed Long-term ice mass changes in Greenland and Antarctica derived from satellite laser ranging [preprint] ...
title_sort long-term ice mass changes in greenland and antarctica derived from satellite laser ranging [preprint] ...
publisher OMEGA-PSIR
publishDate 2024
url https://dx.doi.org/10.57755/xnaf-mv77
https://bazawiedzy.upwr.edu.pl/info/article/UPWR8eeb3a088ebd474695b68fcffdec7929/
genre Antarc*
Antarctica
Greenland
Ice Sheet
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
op_relation https://bazawiedzy.upwr.edu.pl/info/journalseries/WUT64574/
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57755/xnaf-mv77
_version_ 1797574099312050176