GNSS Measurements of GIA-driven crustal deformation in Antarctica
Continuously recording GPS stations have operated at permanent Antarctic research stations, mainly along the coast, for nearly 3 decades. In contrast, deployment of continuously recording autonomous GPS instruments in the continental interior of Antarctica started mainly during the 2007-08 Internati...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018618 2023-09-05T13:15:18+02:00 GNSS Measurements of GIA-driven crustal deformation in Antarctica Wilson, T. Whitehouse, P. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018618 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2206 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018618 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2206 2023-08-13T23:41:24Z Continuously recording GPS stations have operated at permanent Antarctic research stations, mainly along the coast, for nearly 3 decades. In contrast, deployment of continuously recording autonomous GPS instruments in the continental interior of Antarctica started mainly during the 2007-08 International Polar Year. At present, the U.S. ANET-POLENET and UK-ANET projects maintain most GNSS stations across interior and remote coastal West Antarctica and the Antarctic Peninsula; these projects have limited-term support and are currently scheduled to end within the next 2 years. Cessation of data acquisition, due to lack of operational support and/or site decommissioning, is resulting in a crucial gap in observational constraints for GIA modeling. It also hinders a range of studies using GNSS data, spanning the deep Earth to the ionosphere. Geodetic time series from autonomous GNSS systems distributed across Antarctica have revealed unexpected patterns and startling rates of crustal deformation due to GIA. Linked with seismic mapping and derived rheological properties of the Antarctic crust and mantle, and with new advances in GIA modeling capabilities, GNSS observations have transformed our understanding of the timescales of GIA response to ice sheet change. Rapid GIA response promotes cryosphere-solid earth interactions that can alter ice sheet behavior on decadal and centennial timescales, with significant implications for the contributions of marine-based sectors of the Antarctic Ice Sheet to sea level in the future. Continued progress in understanding how such feedbacks should be adopted in global sea level projections requires continuing and expanding our geodetic observations through international cooperation. Conference Object Antarc* Antarctic Antarctic Peninsula Antarctica Ice Sheet International Polar Year West Antarctica GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Anet ENVELOPE(27.987,27.987,65.920,65.920) Antarctic Antarctic Peninsula The Antarctic West Antarctica |
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Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
Continuously recording GPS stations have operated at permanent Antarctic research stations, mainly along the coast, for nearly 3 decades. In contrast, deployment of continuously recording autonomous GPS instruments in the continental interior of Antarctica started mainly during the 2007-08 International Polar Year. At present, the U.S. ANET-POLENET and UK-ANET projects maintain most GNSS stations across interior and remote coastal West Antarctica and the Antarctic Peninsula; these projects have limited-term support and are currently scheduled to end within the next 2 years. Cessation of data acquisition, due to lack of operational support and/or site decommissioning, is resulting in a crucial gap in observational constraints for GIA modeling. It also hinders a range of studies using GNSS data, spanning the deep Earth to the ionosphere. Geodetic time series from autonomous GNSS systems distributed across Antarctica have revealed unexpected patterns and startling rates of crustal deformation due to GIA. Linked with seismic mapping and derived rheological properties of the Antarctic crust and mantle, and with new advances in GIA modeling capabilities, GNSS observations have transformed our understanding of the timescales of GIA response to ice sheet change. Rapid GIA response promotes cryosphere-solid earth interactions that can alter ice sheet behavior on decadal and centennial timescales, with significant implications for the contributions of marine-based sectors of the Antarctic Ice Sheet to sea level in the future. Continued progress in understanding how such feedbacks should be adopted in global sea level projections requires continuing and expanding our geodetic observations through international cooperation. |
format |
Conference Object |
author |
Wilson, T. Whitehouse, P. |
spellingShingle |
Wilson, T. Whitehouse, P. GNSS Measurements of GIA-driven crustal deformation in Antarctica |
author_facet |
Wilson, T. Whitehouse, P. |
author_sort |
Wilson, T. |
title |
GNSS Measurements of GIA-driven crustal deformation in Antarctica |
title_short |
GNSS Measurements of GIA-driven crustal deformation in Antarctica |
title_full |
GNSS Measurements of GIA-driven crustal deformation in Antarctica |
title_fullStr |
GNSS Measurements of GIA-driven crustal deformation in Antarctica |
title_full_unstemmed |
GNSS Measurements of GIA-driven crustal deformation in Antarctica |
title_sort |
gnss measurements of gia-driven crustal deformation in antarctica |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018618 |
long_lat |
ENVELOPE(27.987,27.987,65.920,65.920) |
geographic |
Anet Antarctic Antarctic Peninsula The Antarctic West Antarctica |
geographic_facet |
Anet Antarctic Antarctic Peninsula The Antarctic West Antarctica |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Ice Sheet International Polar Year West Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Ice Sheet International Polar Year West Antarctica |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2206 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018618 |
op_doi |
https://doi.org/10.57757/IUGG23-2206 |
_version_ |
1776197108513112064 |