Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS
In this study, we estimate the ice mass changes, the ice elevation changes and the vertical displacements in Antarctica based on analysis of multi-geodetic datasets that involve the satellite gravimetry (GRACE), the satellite altimetry (ICESat) and the global navigation satellite systems (GNSS). Acc...
Published in: | Contributions to Geophysics and Geodesy |
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Earth Science Institute, Slovak Academy of Sciences, Slovakia
2019
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Online Access: | https://doi.org/10.2478/congeo-2019-0021 https://doaj.org/article/be9c6de0c8e34ecbbfd2a89ef8111246 |
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ftdoajarticles:oai:doaj.org/article:be9c6de0c8e34ecbbfd2a89ef8111246 2023-05-15T13:24:15+02:00 Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS Fang ZOU Robert TENZER Samurdhika RATHNAYAKE 2019-12-01T00:00:00Z https://doi.org/10.2478/congeo-2019-0021 https://doaj.org/article/be9c6de0c8e34ecbbfd2a89ef8111246 EN eng Earth Science Institute, Slovak Academy of Sciences, Slovakia https://journal.geo.sav.sk/cgg/article/view/213 https://doaj.org/toc/1338-0540 1338-0540 doi:10.2478/congeo-2019-0021 https://doaj.org/article/be9c6de0c8e34ecbbfd2a89ef8111246 Contributions to Geophysics and Geodesy, Vol 49, Iss 4, Pp 403-424 (2019) antarctica ice sheet glacier grace icesat Geodesy QB275-343 Geophysics. Cosmic physics QC801-809 article 2019 ftdoajarticles https://doi.org/10.2478/congeo-2019-0021 2022-12-31T02:53:00Z In this study, we estimate the ice mass changes, the ice elevation changes and the vertical displacements in Antarctica based on analysis of multi-geodetic datasets that involve the satellite gravimetry (GRACE), the satellite altimetry (ICESat) and the global navigation satellite systems (GNSS). According to our estimates, the total mass change of the Antarctic ice sheet from GRACE data is −162.91 Gt/yr over the investigated period between April 2002 and June 2017. This value was obtained after applying the GIA correction of −98.12 Gt/yr derived from the ICE-5G model of the glacial isostatic adjustment. A more detailed analysis of mass balance changes for three individual drainage regions in Antarctica reveal that the mass loss of the West Antarctic ice sheet was at a rate of −143.11 Gt/yr. The mass loss of the Antarctic Peninsula ice sheet was at a rate of −24.31 Gt/yr. The mass of the East Antarctic ice sheet increased at a rate of 5.29 Gt/yr during the investigated period. When integrated over the entire Antarctic ice sheet, average rates of ice elevation changes over the period from March 2003 to October 2009 derived from ICESat data represent the loss of total ice volume of −155.6 km3. The most prominent features in ice volume changes in Antarctica are characterized by a strong dynamic thinning and ice mass loss in the Amundsen Sea Embayment that is part of the West Antarctic ice sheet. In contrast, coastal regions between Dronning Maud Land and Enderby Land exhibit a minor ice increase, while a minor ice mass loss is observed in Wilkes Land. The vertical load displacement rates estimated from GRACE and GPS data relatively closely agree with the GIA model derived based on the ice-load history and the viscosity profile. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctic Peninsula Antarctica Dronning Maud Land Enderby Land Ice Sheet Wilkes Land Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Antarctic Peninsula Dronning Maud Land Amundsen Sea West Antarctic Ice Sheet East Antarctic Ice Sheet Wilkes Land ENVELOPE(120.000,120.000,-69.000,-69.000) Contributions to Geophysics and Geodesy 49 4 403 424 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
antarctica ice sheet glacier grace icesat Geodesy QB275-343 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
antarctica ice sheet glacier grace icesat Geodesy QB275-343 Geophysics. Cosmic physics QC801-809 Fang ZOU Robert TENZER Samurdhika RATHNAYAKE Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
topic_facet |
antarctica ice sheet glacier grace icesat Geodesy QB275-343 Geophysics. Cosmic physics QC801-809 |
description |
In this study, we estimate the ice mass changes, the ice elevation changes and the vertical displacements in Antarctica based on analysis of multi-geodetic datasets that involve the satellite gravimetry (GRACE), the satellite altimetry (ICESat) and the global navigation satellite systems (GNSS). According to our estimates, the total mass change of the Antarctic ice sheet from GRACE data is −162.91 Gt/yr over the investigated period between April 2002 and June 2017. This value was obtained after applying the GIA correction of −98.12 Gt/yr derived from the ICE-5G model of the glacial isostatic adjustment. A more detailed analysis of mass balance changes for three individual drainage regions in Antarctica reveal that the mass loss of the West Antarctic ice sheet was at a rate of −143.11 Gt/yr. The mass loss of the Antarctic Peninsula ice sheet was at a rate of −24.31 Gt/yr. The mass of the East Antarctic ice sheet increased at a rate of 5.29 Gt/yr during the investigated period. When integrated over the entire Antarctic ice sheet, average rates of ice elevation changes over the period from March 2003 to October 2009 derived from ICESat data represent the loss of total ice volume of −155.6 km3. The most prominent features in ice volume changes in Antarctica are characterized by a strong dynamic thinning and ice mass loss in the Amundsen Sea Embayment that is part of the West Antarctic ice sheet. In contrast, coastal regions between Dronning Maud Land and Enderby Land exhibit a minor ice increase, while a minor ice mass loss is observed in Wilkes Land. The vertical load displacement rates estimated from GRACE and GPS data relatively closely agree with the GIA model derived based on the ice-load history and the viscosity profile. |
format |
Article in Journal/Newspaper |
author |
Fang ZOU Robert TENZER Samurdhika RATHNAYAKE |
author_facet |
Fang ZOU Robert TENZER Samurdhika RATHNAYAKE |
author_sort |
Fang ZOU |
title |
Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
title_short |
Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
title_full |
Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
title_fullStr |
Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
title_full_unstemmed |
Monitoring changes of the Antarctic Ice sheet by GRACE, ICESat and GNSS |
title_sort |
monitoring changes of the antarctic ice sheet by grace, icesat and gnss |
publisher |
Earth Science Institute, Slovak Academy of Sciences, Slovakia |
publishDate |
2019 |
url |
https://doi.org/10.2478/congeo-2019-0021 https://doaj.org/article/be9c6de0c8e34ecbbfd2a89ef8111246 |
long_lat |
ENVELOPE(120.000,120.000,-69.000,-69.000) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Dronning Maud Land Amundsen Sea West Antarctic Ice Sheet East Antarctic Ice Sheet Wilkes Land |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Dronning Maud Land Amundsen Sea West Antarctic Ice Sheet East Antarctic Ice Sheet Wilkes Land |
genre |
Amundsen Sea Antarc* Antarctic Antarctic Peninsula Antarctica Dronning Maud Land Enderby Land Ice Sheet Wilkes Land |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctic Peninsula Antarctica Dronning Maud Land Enderby Land Ice Sheet Wilkes Land |
op_source |
Contributions to Geophysics and Geodesy, Vol 49, Iss 4, Pp 403-424 (2019) |
op_relation |
https://journal.geo.sav.sk/cgg/article/view/213 https://doaj.org/toc/1338-0540 1338-0540 doi:10.2478/congeo-2019-0021 https://doaj.org/article/be9c6de0c8e34ecbbfd2a89ef8111246 |
op_doi |
https://doi.org/10.2478/congeo-2019-0021 |
container_title |
Contributions to Geophysics and Geodesy |
container_volume |
49 |
container_issue |
4 |
container_start_page |
403 |
op_container_end_page |
424 |
_version_ |
1766378275422076928 |