Bayesian surface wave dispersion inversion of glaciated environments

We present a probabilistic approach to the inversion of surface wave dispersion data from glacial environments. This is intended to (i) assess non-linearity and non-uniqueness, and (ii) properly quantify resolution and trade-offs. For this, we use seismic data from Distributed Acoustic Sensing (DAS)...

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Main Authors: Lanteri, A., Gebraad, L., Zunino, A., Klaasen, S., Jonsdottir, K., Hofstede, C., Eisen, O., Zigone, D., Fichtner, A.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017627
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017627 2023-10-01T03:56:21+02:00 Bayesian surface wave dispersion inversion of glaciated environments Lanteri, A. Gebraad, L. Zunino, A. Klaasen, S. Jonsdottir, K. Hofstede, C. Eisen, O. Zigone, D. Fichtner, A. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017627 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1912 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017627 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1912 2023-09-03T23:42:30Z We present a probabilistic approach to the inversion of surface wave dispersion data from glacial environments. This is intended to (i) assess non-linearity and non-uniqueness, and (ii) properly quantify resolution and trade-offs. For this, we use seismic data from Distributed Acoustic Sensing (DAS) experiments deployed on the Vatnajökull ice sheet located on Grímsvötn volcano in Iceland, and the Northeast Greenland Ice Stream (NEGIS). Our method is based on a regularisation-free Bayesian inference approach, implemented using a Hamiltonian Monte Carlo (HMC) algorithm. Exploiting derivative information for efficient sampling of high-dimensional model spaces, HMC approximates the posterior probability densities of all model parameters. Applied specifically to multi-mode surface wave dispersion measurements, HMC yields probabilistic models of 1-D anisotropic stratified media parameterised in terms of the P-wave velocities Vpv and Vph, the S-wave velocities Vsv and Vsh, the anisotropy parameter η, and density ρ. The benefits of this approach, not only from a glaciological perspective, include regularisation-free estimates of firn and ice properties, models that are not a priori biased by the exclusion of all parameters except S-wave speed, and some level of direct access to the vertical density profile. Conference Object Greenland Ice Sheet Iceland Vatnajökull GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Greenland Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description We present a probabilistic approach to the inversion of surface wave dispersion data from glacial environments. This is intended to (i) assess non-linearity and non-uniqueness, and (ii) properly quantify resolution and trade-offs. For this, we use seismic data from Distributed Acoustic Sensing (DAS) experiments deployed on the Vatnajökull ice sheet located on Grímsvötn volcano in Iceland, and the Northeast Greenland Ice Stream (NEGIS). Our method is based on a regularisation-free Bayesian inference approach, implemented using a Hamiltonian Monte Carlo (HMC) algorithm. Exploiting derivative information for efficient sampling of high-dimensional model spaces, HMC approximates the posterior probability densities of all model parameters. Applied specifically to multi-mode surface wave dispersion measurements, HMC yields probabilistic models of 1-D anisotropic stratified media parameterised in terms of the P-wave velocities Vpv and Vph, the S-wave velocities Vsv and Vsh, the anisotropy parameter η, and density ρ. The benefits of this approach, not only from a glaciological perspective, include regularisation-free estimates of firn and ice properties, models that are not a priori biased by the exclusion of all parameters except S-wave speed, and some level of direct access to the vertical density profile.
format Conference Object
author Lanteri, A.
Gebraad, L.
Zunino, A.
Klaasen, S.
Jonsdottir, K.
Hofstede, C.
Eisen, O.
Zigone, D.
Fichtner, A.
spellingShingle Lanteri, A.
Gebraad, L.
Zunino, A.
Klaasen, S.
Jonsdottir, K.
Hofstede, C.
Eisen, O.
Zigone, D.
Fichtner, A.
Bayesian surface wave dispersion inversion of glaciated environments
author_facet Lanteri, A.
Gebraad, L.
Zunino, A.
Klaasen, S.
Jonsdottir, K.
Hofstede, C.
Eisen, O.
Zigone, D.
Fichtner, A.
author_sort Lanteri, A.
title Bayesian surface wave dispersion inversion of glaciated environments
title_short Bayesian surface wave dispersion inversion of glaciated environments
title_full Bayesian surface wave dispersion inversion of glaciated environments
title_fullStr Bayesian surface wave dispersion inversion of glaciated environments
title_full_unstemmed Bayesian surface wave dispersion inversion of glaciated environments
title_sort bayesian surface wave dispersion inversion of glaciated environments
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017627
long_lat ENVELOPE(-16.823,-16.823,64.420,64.420)
geographic Greenland
Vatnajökull
geographic_facet Greenland
Vatnajökull
genre Greenland
Ice Sheet
Iceland
Vatnajökull
genre_facet Greenland
Ice Sheet
Iceland
Vatnajökull
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1912
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017627
op_doi https://doi.org/10.57757/IUGG23-1912
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