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...

Full description

Bibliographic Details
Published in:Geosciences
Main Authors: 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)
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://resolver.tudelft.nl/uuid:f296f7f2-4ff2-4a1d-b434-ecc63e070494
https://doi.org/10.3390/geosciences9100415
_version_ 1821769288084619264
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