Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...

Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberation...

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Main Authors: Harpley, Dale, Hearn, Steve, Strong, Shaun
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2021
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.6586202
https://zenodo.org/record/6586202
id ftdatacite:10.5281/zenodo.6586202
record_format openpolar
spelling ftdatacite:10.5281/zenodo.6586202 2023-05-15T14:13:46+02:00 Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ... Harpley, Dale Hearn, Steve Strong, Shaun 2021 https://dx.doi.org/10.5281/zenodo.6586202 https://zenodo.org/record/6586202 en eng Zenodo https://zenodo.org/communities/aseg_extended_abstracts_2021 https://dx.doi.org/10.5281/zenodo.6586203 https://zenodo.org/communities/aseg_extended_abstracts_2021 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess receiver function ice-sheet reverberations Wiener filtering predictive deconvolution Article ConferencePaper 2021 ftdatacite https://doi.org/10.5281/zenodo.658620210.5281/zenodo.6586203 2023-04-03T13:08:57Z Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberations can, however, be exploited. We describe a practical process, incorporating a simple generalised linear inversion (GLI) stage, which yields an ice-sheet model. The derived ice model can then be used to design a Wiener filter aimed at attenuating ice phases, and revealing crustal phases in the PRF. Although it is theoretically approximate, the Wiener approach appears robust. Synthetic trialling, using realistic models, is essential for understanding the limitations of the algorithm. The full process has been applied at ice-covered stations in Antarctica and Greenland. In each case, we have derived robust models for the ice, and have successfully extracted crustal Ps phases from the contaminated receiver functions. ... : Open-Access Online Publication: March 03, 2023 ... Article in Journal/Newspaper Antarc* Antarctica Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
spellingShingle receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
Harpley, Dale
Hearn, Steve
Strong, Shaun
Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
topic_facet receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
description Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberations can, however, be exploited. We describe a practical process, incorporating a simple generalised linear inversion (GLI) stage, which yields an ice-sheet model. The derived ice model can then be used to design a Wiener filter aimed at attenuating ice phases, and revealing crustal phases in the PRF. Although it is theoretically approximate, the Wiener approach appears robust. Synthetic trialling, using realistic models, is essential for understanding the limitations of the algorithm. The full process has been applied at ice-covered stations in Antarctica and Greenland. In each case, we have derived robust models for the ice, and have successfully extracted crustal Ps phases from the contaminated receiver functions. ... : Open-Access Online Publication: March 03, 2023 ...
format Article in Journal/Newspaper
author Harpley, Dale
Hearn, Steve
Strong, Shaun
author_facet Harpley, Dale
Hearn, Steve
Strong, Shaun
author_sort Harpley, Dale
title Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
title_short Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
title_full Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
title_fullStr Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
title_full_unstemmed Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions ...
title_sort attenuation of ice-sheet reverberations in teleseismic p-wave receiver functions ...
publisher Zenodo
publishDate 2021
url https://dx.doi.org/10.5281/zenodo.6586202
https://zenodo.org/record/6586202
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
Ice Sheet
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
op_relation https://zenodo.org/communities/aseg_extended_abstracts_2021
https://dx.doi.org/10.5281/zenodo.6586203
https://zenodo.org/communities/aseg_extended_abstracts_2021
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.658620210.5281/zenodo.6586203
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