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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Main Authors: Wilson, T., Whitehouse, P.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018618
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spelling 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
institution 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
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