Extraction and applications of Rayleigh wave ellipticity in polar regions
Seismic Rayleigh wave ellipticity measurements are the horizontal-to-vertical ratio of the Rayleigh wave particle motion, and are sensitive to the subsurface structure beneath a seismic station. H/V ratios measured from the ambient vibrations of the Earth are being increasingly used in glaciological...
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2023
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Online Access: | http://hdl.handle.net/10261/361092 https://doi.org/10.1017/aog.2023.1 |
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ftcsic:oai:digital.csic.es:10261/361092 2024-09-09T19:01:03+00:00 Extraction and applications of Rayleigh wave ellipticity in polar regions Jones, Glenn A. Kulessa, Bernd Ferreira, A. M. G. Schimmel, Martin Berbellini, Andrea Morelli, Andrea European Commission Agencia Estatal de Investigación (España) 2023 http://hdl.handle.net/10261/361092 https://doi.org/10.1017/aog.2023.1 unknown Cambridge University Press #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-095594-B-I00/ES/MONITORIZACION DE ESTRUCTURAS GEOLOGICAS SUPERFICIALES MEDIANTE EL ANALISIS DEL RUIDO SISMICO AMBIENTE/ Publisher's version http://dx.doi.org/10.1017/aog.2023.1 Sí doi:10.1017/aog.2023.1 issn: 1727-5644 Annals of Glaciology, 63: 3- 7 (2023) http://hdl.handle.net/10261/361092 open Glacier geophysics Glacier monitoring Sea-ice geophysics Seismology artículo 2023 ftcsic https://doi.org/10.1017/aog.2023.1 2024-06-26T00:01:43Z Seismic Rayleigh wave ellipticity measurements are the horizontal-to-vertical ratio of the Rayleigh wave particle motion, and are sensitive to the subsurface structure beneath a seismic station. H/V ratios measured from the ambient vibrations of the Earth are being increasingly used in glaciological applications to determine glacier and ice sheet thickness, seismic velocities and firn properties. Using the newly developed degree-of-polarisation (DOP-E) method which exploits the polarisation properties of seismic noise, we identify and extract Rayleigh waves from seismic stations in Greenland, and relate them to sea ice processes and the geology of the upper crust. Finally, we provide some suggestions for future applications of DOP-E method to gain greater insight into seasonal and long-term variability of sea ice formation and breakup as well as the monitoring of ice sheet thickness, subglacial environment and firn layers in the poles. G.A.J. is funded through the by the Sêr Cymru II Program in Low Carbon Energy and the Environment (European Regional Development Fund and Welsh European Funding Office; Project number 80761-SU-SU093). A.M.G.F. is grateful to support from NERC grant NE/N011791/1. M.S. thanks SANIMS (RTI2018-095594-B-I00). This project has received funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement No 101001601). Article in Journal/Newspaper Annals of Glaciology glacier Greenland Ice Sheet Sea ice Digital.CSIC (Spanish National Research Council) Greenland Annals of Glaciology 63 87-89 3 7 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
unknown |
topic |
Glacier geophysics Glacier monitoring Sea-ice geophysics Seismology |
spellingShingle |
Glacier geophysics Glacier monitoring Sea-ice geophysics Seismology Jones, Glenn A. Kulessa, Bernd Ferreira, A. M. G. Schimmel, Martin Berbellini, Andrea Morelli, Andrea Extraction and applications of Rayleigh wave ellipticity in polar regions |
topic_facet |
Glacier geophysics Glacier monitoring Sea-ice geophysics Seismology |
description |
Seismic Rayleigh wave ellipticity measurements are the horizontal-to-vertical ratio of the Rayleigh wave particle motion, and are sensitive to the subsurface structure beneath a seismic station. H/V ratios measured from the ambient vibrations of the Earth are being increasingly used in glaciological applications to determine glacier and ice sheet thickness, seismic velocities and firn properties. Using the newly developed degree-of-polarisation (DOP-E) method which exploits the polarisation properties of seismic noise, we identify and extract Rayleigh waves from seismic stations in Greenland, and relate them to sea ice processes and the geology of the upper crust. Finally, we provide some suggestions for future applications of DOP-E method to gain greater insight into seasonal and long-term variability of sea ice formation and breakup as well as the monitoring of ice sheet thickness, subglacial environment and firn layers in the poles. G.A.J. is funded through the by the Sêr Cymru II Program in Low Carbon Energy and the Environment (European Regional Development Fund and Welsh European Funding Office; Project number 80761-SU-SU093). A.M.G.F. is grateful to support from NERC grant NE/N011791/1. M.S. thanks SANIMS (RTI2018-095594-B-I00). This project has received funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement No 101001601). |
author2 |
European Commission Agencia Estatal de Investigación (España) |
format |
Article in Journal/Newspaper |
author |
Jones, Glenn A. Kulessa, Bernd Ferreira, A. M. G. Schimmel, Martin Berbellini, Andrea Morelli, Andrea |
author_facet |
Jones, Glenn A. Kulessa, Bernd Ferreira, A. M. G. Schimmel, Martin Berbellini, Andrea Morelli, Andrea |
author_sort |
Jones, Glenn A. |
title |
Extraction and applications of Rayleigh wave ellipticity in polar regions |
title_short |
Extraction and applications of Rayleigh wave ellipticity in polar regions |
title_full |
Extraction and applications of Rayleigh wave ellipticity in polar regions |
title_fullStr |
Extraction and applications of Rayleigh wave ellipticity in polar regions |
title_full_unstemmed |
Extraction and applications of Rayleigh wave ellipticity in polar regions |
title_sort |
extraction and applications of rayleigh wave ellipticity in polar regions |
publisher |
Cambridge University Press |
publishDate |
2023 |
url |
http://hdl.handle.net/10261/361092 https://doi.org/10.1017/aog.2023.1 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Annals of Glaciology glacier Greenland Ice Sheet Sea ice |
genre_facet |
Annals of Glaciology glacier Greenland Ice Sheet Sea ice |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-095594-B-I00/ES/MONITORIZACION DE ESTRUCTURAS GEOLOGICAS SUPERFICIALES MEDIANTE EL ANALISIS DEL RUIDO SISMICO AMBIENTE/ Publisher's version http://dx.doi.org/10.1017/aog.2023.1 Sí doi:10.1017/aog.2023.1 issn: 1727-5644 Annals of Glaciology, 63: 3- 7 (2023) http://hdl.handle.net/10261/361092 |
op_rights |
open |
op_doi |
https://doi.org/10.1017/aog.2023.1 |
container_title |
Annals of Glaciology |
container_volume |
63 |
container_issue |
87-89 |
container_start_page |
3 |
op_container_end_page |
7 |
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1809943296573702144 |