Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results
Satellite gravimetry data acquired by the Gravity Recovery and Climate Experiment (GRACE) allows to derive the temporal evolution in ice mass for both the Antarctic Ice Sheet (AIS) and the Greenland Ice Sheet (GIS). Various algorithms have been used in a wide range of studies to generate Gravimetric...
Published in: | Geosciences |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 https://doi.org/10.3390/geosciences9100415 |
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author | Groh, Andreas (author) Horwath, Martin (author) Horvath, Alexander (author) Meister, Rakia (author) Wouters, B. (author) Ditmar, P.G. (author) Ran, J. (author) Klees, R. (author) Schrama, Ernst (author) |
author_facet | Groh, Andreas (author) Horwath, Martin (author) Horvath, Alexander (author) Meister, Rakia (author) Wouters, B. (author) Ditmar, P.G. (author) Ran, J. (author) Klees, R. (author) Schrama, Ernst (author) |
author_sort | Groh, Andreas (author) |
collection | Delft University of Technology: Institutional Repository |
container_issue | 10 |
container_start_page | 415 |
container_title | Geosciences |
container_volume | 9 |
description | Satellite gravimetry data acquired by the Gravity Recovery and Climate Experiment (GRACE) allows to derive the temporal evolution in ice mass for both the Antarctic Ice Sheet (AIS) and the Greenland Ice Sheet (GIS). Various algorithms have been used in a wide range of studies to generate Gravimetric Mass Balance (GMB) products. Results from different studies may be affected by substantial differences in the processing, including the applied algorithm, the utilised background models and the time period under consideration. This study gives a detailed description of an assessment of the performance of GMB algorithms using actual GRACE monthly solutions for a prescribed period as well as synthetic data sets. The inter-comparison exercise was conducted in the scope of the European Space Agency’s Climate Change Initiative (CCI) project for the AIS and GIS, and was, for the first time, open to everyone. GMB products generated by different groups could be evaluated and directly compared against each other. For the period from 2003-02 to 2013-12, estimated linear trends in ice mass vary between −99 Gt/yr and −108 Gt/yr for the AIS and between −252 Gt/yr and −274 Gt/yr for the GIS, respectively. The spread between the solutions is larger if smaller drainage basins or gridded GMB products are considered. Finally, findings from the exercise formed the basis to select the algorithms used for the GMB product generation within the AIS and GIS CCI project. Physical and Space Geodesy Astrodynamics & Space Missions |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctica Greenland Ice Sheet |
genre_facet | Antarc* Antarctic Antarctica Greenland Ice Sheet |
geographic | Antarctic Greenland The Antarctic |
geographic_facet | Antarctic Greenland The Antarctic |
id | fttudelft:oai:tudelft.nl:uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 |
institution | Open Polar |
language | English |
op_collection_id | fttudelft |
op_doi | https://doi.org/10.3390/geosciences9100415 |
op_relation | https://www.mdpi.com/2076-3263/9/10/415 http://www.scopus.com/inward/record.url?scp=85073453027&partnerID=8YFLogxK Geosciences (Switzerland)--2076-3263--00f0e33c-992c-4f4f-8502-c9b9166d74ae http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 https://doi.org/10.3390/geosciences9100415 |
op_rights | © 2019 Andreas Groh, Martin Horwath, Alexander Horvath, Rakia Meister, B. Wouters, P.G. Ditmar, J. Ran, R. Klees, Ernst Schrama, More Authors |
publishDate | 2019 |
record_format | openpolar |
spelling | fttudelft:oai:tudelft.nl:uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 2025-01-16T19:36:17+00:00 Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results Groh, Andreas (author) Horwath, Martin (author) Horvath, Alexander (author) Meister, Rakia (author) Wouters, B. (author) Ditmar, P.G. (author) Ran, J. (author) Klees, R. (author) Schrama, Ernst (author) 2019 http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 https://doi.org/10.3390/geosciences9100415 en eng https://www.mdpi.com/2076-3263/9/10/415 http://www.scopus.com/inward/record.url?scp=85073453027&partnerID=8YFLogxK Geosciences (Switzerland)--2076-3263--00f0e33c-992c-4f4f-8502-c9b9166d74ae http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 https://doi.org/10.3390/geosciences9100415 © 2019 Andreas Groh, Martin Horwath, Alexander Horvath, Rakia Meister, B. Wouters, P.G. Ditmar, J. Ran, R. Klees, Ernst Schrama, More Authors Antarctica GRACE Greenland Ice mass change Methods journal article 2019 fttudelft https://doi.org/10.3390/geosciences9100415 2024-04-09T23:55:06Z Satellite gravimetry data acquired by the Gravity Recovery and Climate Experiment (GRACE) allows to derive the temporal evolution in ice mass for both the Antarctic Ice Sheet (AIS) and the Greenland Ice Sheet (GIS). Various algorithms have been used in a wide range of studies to generate Gravimetric Mass Balance (GMB) products. Results from different studies may be affected by substantial differences in the processing, including the applied algorithm, the utilised background models and the time period under consideration. This study gives a detailed description of an assessment of the performance of GMB algorithms using actual GRACE monthly solutions for a prescribed period as well as synthetic data sets. The inter-comparison exercise was conducted in the scope of the European Space Agency’s Climate Change Initiative (CCI) project for the AIS and GIS, and was, for the first time, open to everyone. GMB products generated by different groups could be evaluated and directly compared against each other. For the period from 2003-02 to 2013-12, estimated linear trends in ice mass vary between −99 Gt/yr and −108 Gt/yr for the AIS and between −252 Gt/yr and −274 Gt/yr for the GIS, respectively. The spread between the solutions is larger if smaller drainage basins or gridded GMB products are considered. Finally, findings from the exercise formed the basis to select the algorithms used for the GMB product generation within the AIS and GIS CCI project. Physical and Space Geodesy Astrodynamics & Space Missions Article in Journal/Newspaper Antarc* Antarctic Antarctica Greenland Ice Sheet Delft University of Technology: Institutional Repository Antarctic Greenland The Antarctic Geosciences 9 10 415 |
spellingShingle | Antarctica GRACE Greenland Ice mass change Methods Groh, Andreas (author) Horwath, Martin (author) Horvath, Alexander (author) Meister, Rakia (author) Wouters, B. (author) Ditmar, P.G. (author) Ran, J. (author) Klees, R. (author) Schrama, Ernst (author) Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title | Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title_full | Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title_fullStr | Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title_full_unstemmed | Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title_short | Evaluating GRACE Mass Change Time Series for the Antarctic and Greenland Ice Sheet—Methods and Results |
title_sort | evaluating grace mass change time series for the antarctic and greenland ice sheet—methods and results |
topic | Antarctica GRACE Greenland Ice mass change Methods |
topic_facet | Antarctica GRACE Greenland Ice mass change Methods |
url | http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494 https://doi.org/10.3390/geosciences9100415 |