Global glacier mass loss during the GRACE satellite mission (2002-2016)
Glaciers outside of the ice sheets are known to be important contributors to sea level rise. In this work, we provide an overview of changes in the mass of the world's glaciers, excluding those in Greenland and Antarctica, between 2002 and 2016, based on satellite gravimetry observations of the...
Published in: | Frontiers in Earth Science |
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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:cf653f45-3c77-4114-8d37-e409ae9e7f58 https://doi.org/10.3389/feart.2019.00096 |
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author | Wouters, B. (author) Gardner, Alex S. (author) Moholdt, Geir (author) |
author_facet | Wouters, B. (author) Gardner, Alex S. (author) Moholdt, Geir (author) |
author_sort | Wouters, B. (author) |
collection | Delft University of Technology: Institutional Repository |
container_title | Frontiers in Earth Science |
container_volume | 7 |
description | Glaciers outside of the ice sheets are known to be important contributors to sea level rise. In this work, we provide an overview of changes in the mass of the world's glaciers, excluding those in Greenland and Antarctica, between 2002 and 2016, based on satellite gravimetry observations of the Gravity Recovery and Climate Experiment (GRACE). Glaciers lost mass at a rate of 199 ± 32 Gt yr −1 during this 14-yr period, equivalent to a cumulative sea level contribution of 8 mm. We present annual mass balances for 17 glacier regions, that show a qualitatively good agreement with published estimates from in situ observations. We find that annual mass balance varies considerably from year to year, which can in part be attributed to changes in the large-scale circulation of the atmosphere. These variations, combined with the relatively short observational record, hamper the detection of acceleration of glacier mass loss. Our study highlights the need for continued observations of the Earth's glacierized regions. Physical and Space Geodesy |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctica glacier Greenland |
genre_facet | Antarc* Antarctica glacier Greenland |
geographic | Greenland |
geographic_facet | Greenland |
id | fttudelft:oai:tudelft.nl:uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 |
institution | Open Polar |
language | English |
op_collection_id | fttudelft |
op_doi | https://doi.org/10.3389/feart.2019.00096 |
op_relation | http://www.scopus.com/inward/record.url?scp=85067403009&partnerID=8YFLogxK Frontiers in earth science--2296-6463--9889ff20-d7fd-44c5-a861-f560199d1243 http://resolver.tudelft.nl/uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 https://doi.org/10.3389/feart.2019.00096 |
op_rights | © 2019 B. Wouters, Alex S. Gardner, Geir Moholdt |
publishDate | 2019 |
record_format | openpolar |
spelling | fttudelft:oai:tudelft.nl:uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 2025-01-16T19:34:20+00:00 Global glacier mass loss during the GRACE satellite mission (2002-2016) Wouters, B. (author) Gardner, Alex S. (author) Moholdt, Geir (author) 2019 http://resolver.tudelft.nl/uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 https://doi.org/10.3389/feart.2019.00096 en eng http://www.scopus.com/inward/record.url?scp=85067403009&partnerID=8YFLogxK Frontiers in earth science--2296-6463--9889ff20-d7fd-44c5-a861-f560199d1243 http://resolver.tudelft.nl/uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 https://doi.org/10.3389/feart.2019.00096 © 2019 B. Wouters, Alex S. Gardner, Geir Moholdt GRACE Glaciers Ice caps Mass balance Sea level journal article 2019 fttudelft https://doi.org/10.3389/feart.2019.00096 2024-04-09T23:55:06Z Glaciers outside of the ice sheets are known to be important contributors to sea level rise. In this work, we provide an overview of changes in the mass of the world's glaciers, excluding those in Greenland and Antarctica, between 2002 and 2016, based on satellite gravimetry observations of the Gravity Recovery and Climate Experiment (GRACE). Glaciers lost mass at a rate of 199 ± 32 Gt yr −1 during this 14-yr period, equivalent to a cumulative sea level contribution of 8 mm. We present annual mass balances for 17 glacier regions, that show a qualitatively good agreement with published estimates from in situ observations. We find that annual mass balance varies considerably from year to year, which can in part be attributed to changes in the large-scale circulation of the atmosphere. These variations, combined with the relatively short observational record, hamper the detection of acceleration of glacier mass loss. Our study highlights the need for continued observations of the Earth's glacierized regions. Physical and Space Geodesy Article in Journal/Newspaper Antarc* Antarctica glacier Greenland Delft University of Technology: Institutional Repository Greenland Frontiers in Earth Science 7 |
spellingShingle | GRACE Glaciers Ice caps Mass balance Sea level Wouters, B. (author) Gardner, Alex S. (author) Moholdt, Geir (author) Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title | Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title_full | Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title_fullStr | Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title_full_unstemmed | Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title_short | Global glacier mass loss during the GRACE satellite mission (2002-2016) |
title_sort | global glacier mass loss during the grace satellite mission (2002-2016) |
topic | GRACE Glaciers Ice caps Mass balance Sea level |
topic_facet | GRACE Glaciers Ice caps Mass balance Sea level |
url | http://resolver.tudelft.nl/uuid:cf653f45-3c77-4114-8d37-e409ae9e7f58 https://doi.org/10.3389/feart.2019.00096 |