Monitoring southwest Greenlands ice sheet melt with ambient seismic noise
The Greenland ice sheet presently accounts for ~70% of global ice sheet mass loss. Because this mass loss is associated with sea-level rise at a rate of 0.7 mm/year, the development of improved monitoring techniques to observe ongoing changes in ice sheet mass balance is of paramount concern. Spaceb...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | en_US |
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American Association for the Advancement of Science (AAAS)
2016
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| Online Access: | http://hdl.handle.net/1721.1/102453 https://orcid.org/0000-0002-7998-5417 |
| _version_ | 1826192134052511744 |
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| author | Mordret, Aurelien Mikesell, T. Dylan Harig, Christopher Lipovsky, Bradley P. Prieto Gomez, German A. |
| author2 | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
| author_facet | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Mordret, Aurelien Mikesell, T. Dylan Harig, Christopher Lipovsky, Bradley P. Prieto Gomez, German A. |
| author_sort | Mordret, Aurelien |
| collection | MIT |
| description | The Greenland ice sheet presently accounts for ~70% of global ice sheet mass loss. Because this mass loss is associated with sea-level rise at a rate of 0.7 mm/year, the development of improved monitoring techniques to observe ongoing changes in ice sheet mass balance is of paramount concern. Spaceborne mass balance techniques are commonly used; however, they are inadequate for many purposes because of their low spatial and/or temporal resolution. We demonstrate that small variations in seismic wave speed in Earth’s crust, as measured with the correlation of seismic noise, may be used to infer seasonal ice sheet mass balance. Seasonal loading and unloading of glacial mass induces strain in the crust, and these strains then result in seismic velocity changes due to poroelastic processes. Our method provides a new and independent way of monitoring (in near real time) ice sheet mass balance, yielding new constraints on ice sheet evolution and its contribution to global sea-level changes. An increased number of seismic stations in the vicinity of ice sheets will enhance our ability to create detailed space-time records of ice mass variations. |
| first_indexed | 2024-09-23T09:06:46Z |
| format | Article |
| id | mit-1721.1/102453 |
| institution | Massachusetts Institute of Technology |
| language | en_US |
| last_indexed | 2024-09-23T09:06:46Z |
| publishDate | 2016 |
| publisher | American Association for the Advancement of Science (AAAS) |
| record_format | dspace |
| spelling | mit-1721.1/1024532022-09-30T13:31:43Z Monitoring southwest Greenlands ice sheet melt with ambient seismic noise Mordret, Aurelien Mikesell, T. Dylan Harig, Christopher Lipovsky, Bradley P. Prieto Gomez, German A. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Mordret, Aurelien Mikesell, T. Dylan Prieto Gomez, German A. The Greenland ice sheet presently accounts for ~70% of global ice sheet mass loss. Because this mass loss is associated with sea-level rise at a rate of 0.7 mm/year, the development of improved monitoring techniques to observe ongoing changes in ice sheet mass balance is of paramount concern. Spaceborne mass balance techniques are commonly used; however, they are inadequate for many purposes because of their low spatial and/or temporal resolution. We demonstrate that small variations in seismic wave speed in Earth’s crust, as measured with the correlation of seismic noise, may be used to infer seasonal ice sheet mass balance. Seasonal loading and unloading of glacial mass induces strain in the crust, and these strains then result in seismic velocity changes due to poroelastic processes. Our method provides a new and independent way of monitoring (in near real time) ice sheet mass balance, yielding new constraints on ice sheet evolution and its contribution to global sea-level changes. An increased number of seismic stations in the vicinity of ice sheets will enhance our ability to create detailed space-time records of ice mass variations. National Science Foundation (U.S.) (Grant EAR-1415907) National Science Foundation (U.S.) (Award 1144883) 2016-05-11T17:00:12Z 2016-05-11T17:00:12Z 2016-05 2015-10 Article http://purl.org/eprint/type/JournalArticle 2375-2548 http://hdl.handle.net/1721.1/102453 Mordret, A., T. D. Mikesell, C. Harig, B. P. Lipovsky, and G. A. Prieto. “Monitoring Southwest Greenlands Ice Sheet Melt with Ambient Seismic Noise.” Science Advances 2, no. 5 (May 6, 2016): e1501538–e1501538. https://orcid.org/0000-0002-7998-5417 en_US http://dx.doi.org/10.1126/sciadv.1501538 Science Advances Creative Commons Attribution http://creativecommons.org/licenses/by/4.0/ application/pdf American Association for the Advancement of Science (AAAS) AAAS |
| spellingShingle | Mordret, Aurelien Mikesell, T. Dylan Harig, Christopher Lipovsky, Bradley P. Prieto Gomez, German A. Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title | Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title_full | Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title_fullStr | Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title_full_unstemmed | Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title_short | Monitoring southwest Greenlands ice sheet melt with ambient seismic noise |
| title_sort | monitoring southwest greenlands ice sheet melt with ambient seismic noise |
| url | http://hdl.handle.net/1721.1/102453 https://orcid.org/0000-0002-7998-5417 |
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