Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach

Distributed Acoustic Sensing (DAS) is increasingly recognised as a valuable tool for glaciological seismic applications, although analysing the large data volumes generated in acquisitions poses computational challenges. We show the potential of active-source DAS to image and characterise subglacial...

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Main Authors: Adam D. Booth, Poul Christoffersen, Andrew Pretorius, Joseph Chapman, Bryn Hubbard, Emma C. Smith, Sjoerd de Ridder, Andy Nowacki, Bradley Paul Lipovsky, Marine Denolle
Format: Article
Language:English
Published: Cambridge University Press 2022-09-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305523000150/type/journal_article
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author Adam D. Booth
Poul Christoffersen
Andrew Pretorius
Joseph Chapman
Bryn Hubbard
Emma C. Smith
Sjoerd de Ridder
Andy Nowacki
Bradley Paul Lipovsky
Marine Denolle
author_facet Adam D. Booth
Poul Christoffersen
Andrew Pretorius
Joseph Chapman
Bryn Hubbard
Emma C. Smith
Sjoerd de Ridder
Andy Nowacki
Bradley Paul Lipovsky
Marine Denolle
author_sort Adam D. Booth
collection DOAJ
description Distributed Acoustic Sensing (DAS) is increasingly recognised as a valuable tool for glaciological seismic applications, although analysing the large data volumes generated in acquisitions poses computational challenges. We show the potential of active-source DAS to image and characterise subglacial sediment beneath a fast-flowing Greenlandic outlet glacier, estimating the thickness of sediment layers to be 20–30 m. However, the lack of subglacial velocity constraint limits the accuracy of this estimate. Constraint could be provided by analysing cryoseismic events in a counterpart 3-day record of passive seismicity through, for example, seismic tomography, but locating them within the 9 TB data volume is computationally inefficient. We describe experiments with data compression using the frequency-wavenumber (f-k) transform ahead of training a convolutional neural network, that provides a ~300-fold improvement in efficiency. In combining active and passive-source and our machine learning framework, the potential of large DAS datasets could be unlocked for a range of future applications.
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spelling doaj.art-dc4bddb3fc474f88b97fa3acace74b402023-10-13T10:44:52ZengCambridge University PressAnnals of Glaciology0260-30551727-56442022-09-0163798210.1017/aog.2023.15Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approachAdam D. Booth0Poul Christoffersen1https://orcid.org/0000-0003-2643-8724Andrew Pretorius2Joseph Chapman3Bryn Hubbard4https://orcid.org/0000-0002-3565-3875Emma C. Smith5https://orcid.org/0000-0002-8672-8259Sjoerd de Ridder6Andy Nowacki7https://orcid.org/0000-0001-7669-7383Bradley Paul Lipovsky8https://orcid.org/0000-0003-4940-0745Marine Denolle9School of Earth and Environment, University of Leeds, Leeds, UKScott Polar Research Institute, University of Cambridge, Cambridge, UKSchool of Earth and Environment, University of Leeds, Leeds, UKSchool of Earth and Environment, University of Leeds, Leeds, UKGeography & Earth Sciences, Aberystwyth University, Aberystwyth, UKSchool of Earth and Environment, University of Leeds, Leeds, UKSchool of Earth and Environment, University of Leeds, Leeds, UKSchool of Earth and Environment, University of Leeds, Leeds, UKDepartment of Earth and Space Sciences, University of Washington College of the Environment, Seattle, WA, USADepartment of Earth and Space Sciences, University of Washington College of the Environment, Seattle, WA, USADistributed Acoustic Sensing (DAS) is increasingly recognised as a valuable tool for glaciological seismic applications, although analysing the large data volumes generated in acquisitions poses computational challenges. We show the potential of active-source DAS to image and characterise subglacial sediment beneath a fast-flowing Greenlandic outlet glacier, estimating the thickness of sediment layers to be 20–30 m. However, the lack of subglacial velocity constraint limits the accuracy of this estimate. Constraint could be provided by analysing cryoseismic events in a counterpart 3-day record of passive seismicity through, for example, seismic tomography, but locating them within the 9 TB data volume is computationally inefficient. We describe experiments with data compression using the frequency-wavenumber (f-k) transform ahead of training a convolutional neural network, that provides a ~300-fold improvement in efficiency. In combining active and passive-source and our machine learning framework, the potential of large DAS datasets could be unlocked for a range of future applications.https://www.cambridge.org/core/product/identifier/S0260305523000150/type/journal_articleAnisotropic icearctic glaciologyglaciological instruments and methodsseismologysubglacial sediments
spellingShingle Adam D. Booth
Poul Christoffersen
Andrew Pretorius
Joseph Chapman
Bryn Hubbard
Emma C. Smith
Sjoerd de Ridder
Andy Nowacki
Bradley Paul Lipovsky
Marine Denolle
Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
Annals of Glaciology
Anisotropic ice
arctic glaciology
glaciological instruments and methods
seismology
subglacial sediments
title Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
title_full Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
title_fullStr Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
title_full_unstemmed Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
title_short Characterising sediment thickness beneath a Greenlandic outlet glacier using distributed acoustic sensing: preliminary observations and progress towards an efficient machine learning approach
title_sort characterising sediment thickness beneath a greenlandic outlet glacier using distributed acoustic sensing preliminary observations and progress towards an efficient machine learning approach
topic Anisotropic ice
arctic glaciology
glaciological instruments and methods
seismology
subglacial sediments
url https://www.cambridge.org/core/product/identifier/S0260305523000150/type/journal_article
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