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Utilising seismic station internal GPS for tracking surging glacier sliding velocity

Wojciech Gajek Orcid Logo, Adrian Luckman Orcid Logo, William D. Harcourt Orcid Logo, Danni Mei Pearce Orcid Logo, Richard Hann Orcid Logo

Journal of Glaciology, Volume: 71, Start page: e40

Swansea University Author: Adrian Luckman Orcid Logo

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    © The Author(s), 2025. Published by Cambridge University Press on behalf of International Glaciological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-ShareAlike licence (CC BY-NC-SA).

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DOI (Published version): 10.1017/jog.2025.30

Abstract

Glacier ice flux is a key indicator of mass balance; therefore, accurate monitoring of ice dynamics is essential. Satellite-based methods are widely used for glacier velocity measurements but are limited by satellite revisit frequency. This study explores using seismic station internal GPS data to t...

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Published in: Journal of Glaciology
ISSN: 0022-1430 1727-5652
Published: Cambridge University Press (CUP) 2025
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa70698
Abstract: Glacier ice flux is a key indicator of mass balance; therefore, accurate monitoring of ice dynamics is essential. Satellite-based methods are widely used for glacier velocity measurements but are limited by satellite revisit frequency. This study explores using seismic station internal GPS data to track glacier movement. While less accurate than differential GPS, this method offers high-temporal resolution as a by-product where seismic stations are deployed. Using a seismic station on Borebreen, Svalbard, we show that internal GPS provides reliable surface velocity measurements. When compared with satellite-inferred velocities, the results show a strong correlation, suggesting that the internal GPS, despite its inherent uncertainty, can serve as an efficient tool for glacier velocity monitoring. The high-temporal sampling reveals short-term dynamics of speed-up events and underscores the role of meltwater in driving these processes. This approach augments glacier observation networks at no additional cost.
Item Description: Letter
Keywords: glacier flow, glacier surges, ice velocity, seismology
College: Faculty of Science and Engineering
Funders: We acknowledge funding from the Royal Geographical Society (RGS) Walters Kundert Fellowship, a Norwegian Research Council (RCN) Arctic Field Grant, and from the Svalbard Integrated Arctic Earth Observing System (SIOS) via an access to Planet Imagery grant.
Start Page: e40