Acoustic waveform inversion for ocean turbulence

The seismic oceanography method is based on extracting and stacking the low-frequency acoustic energy scattered by the ocean heterogeneity. However, a good understanding on how this acoustic wavefield is affected by physical processes in the ocean is still lacking. In this work an acoustic waveform...

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Published in:Journal of Physical Oceanography
Main Authors: Minakov, Alexander, Keers, Henk, Kolyukhin, Dmitriy, Tengesdal, Hans Christian
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2018
Subjects:
Online Access:https://hdl.handle.net/1956/19282
https://doi.org/10.1175/jpo-d-16-0236.1
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spelling ftunivbergen:oai:bora.uib.no:1956/19282 2023-05-15T15:39:01+02:00 Acoustic waveform inversion for ocean turbulence Minakov, Alexander Keers, Henk Kolyukhin, Dmitriy Tengesdal, Hans Christian 2018-02-10T14:27:24Z application/pdf https://hdl.handle.net/1956/19282 https://doi.org/10.1175/jpo-d-16-0236.1 eng eng American Meteorological Society Norges forskningsråd: 223272 urn:issn:0022-3670 urn:issn:1520-0485 https://hdl.handle.net/1956/19282 https://doi.org/10.1175/jpo-d-16-0236.1 cristin:1499121 Copyright 2017 American Meteorological Society Journal of Physical Oceanography Peer reviewed Journal article 2018 ftunivbergen https://doi.org/10.1175/jpo-d-16-0236.1 2023-03-14T17:39:29Z The seismic oceanography method is based on extracting and stacking the low-frequency acoustic energy scattered by the ocean heterogeneity. However, a good understanding on how this acoustic wavefield is affected by physical processes in the ocean is still lacking. In this work an acoustic waveform modeling and inversion method is developed and applied to both synthetic and real data. In the synthetic example, the temperature field is simulated as a homogeneous Gaussian isotropic random field with the Kolmogorov–Obukhov spectrum superimposed on a background stratified ocean structure. The presented full waveform inversion method is based on the ray-Born approximation. The synthetic seismograms computed using the ray-Born scattering method closely match the seismograms produced with a more computationally expensive finite-difference method. The efficient solution to the inverse problem is provided by the multiscale nonlinear inversion approach that is specifically stable with respect to noise. Full waveform inversion tests are performed using both the stationary and time-dependent sound speed models. These tests show that the method provides a reliable reconstruction of both the spatial sound speed variation and the theoretical spectrum due to fully developed turbulence. Finally, the inversion approach is applied to real seismic reflection data to determine the heterogeneous sound speed structure at the west Barents Sea continental margin in the northeast Atlantic. The obtained model illustrates in more detail the processes of diapycnal mixing near the continental slope. publishedVersion Article in Journal/Newspaper Barents Sea Northeast Atlantic University of Bergen: Bergen Open Research Archive (BORA-UiB) Barents Sea Journal of Physical Oceanography 47 6 1473 1491
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description The seismic oceanography method is based on extracting and stacking the low-frequency acoustic energy scattered by the ocean heterogeneity. However, a good understanding on how this acoustic wavefield is affected by physical processes in the ocean is still lacking. In this work an acoustic waveform modeling and inversion method is developed and applied to both synthetic and real data. In the synthetic example, the temperature field is simulated as a homogeneous Gaussian isotropic random field with the Kolmogorov–Obukhov spectrum superimposed on a background stratified ocean structure. The presented full waveform inversion method is based on the ray-Born approximation. The synthetic seismograms computed using the ray-Born scattering method closely match the seismograms produced with a more computationally expensive finite-difference method. The efficient solution to the inverse problem is provided by the multiscale nonlinear inversion approach that is specifically stable with respect to noise. Full waveform inversion tests are performed using both the stationary and time-dependent sound speed models. These tests show that the method provides a reliable reconstruction of both the spatial sound speed variation and the theoretical spectrum due to fully developed turbulence. Finally, the inversion approach is applied to real seismic reflection data to determine the heterogeneous sound speed structure at the west Barents Sea continental margin in the northeast Atlantic. The obtained model illustrates in more detail the processes of diapycnal mixing near the continental slope. publishedVersion
format Article in Journal/Newspaper
author Minakov, Alexander
Keers, Henk
Kolyukhin, Dmitriy
Tengesdal, Hans Christian
spellingShingle Minakov, Alexander
Keers, Henk
Kolyukhin, Dmitriy
Tengesdal, Hans Christian
Acoustic waveform inversion for ocean turbulence
author_facet Minakov, Alexander
Keers, Henk
Kolyukhin, Dmitriy
Tengesdal, Hans Christian
author_sort Minakov, Alexander
title Acoustic waveform inversion for ocean turbulence
title_short Acoustic waveform inversion for ocean turbulence
title_full Acoustic waveform inversion for ocean turbulence
title_fullStr Acoustic waveform inversion for ocean turbulence
title_full_unstemmed Acoustic waveform inversion for ocean turbulence
title_sort acoustic waveform inversion for ocean turbulence
publisher American Meteorological Society
publishDate 2018
url https://hdl.handle.net/1956/19282
https://doi.org/10.1175/jpo-d-16-0236.1
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
Northeast Atlantic
genre_facet Barents Sea
Northeast Atlantic
op_source Journal of Physical Oceanography
op_relation Norges forskningsråd: 223272
urn:issn:0022-3670
urn:issn:1520-0485
https://hdl.handle.net/1956/19282
https://doi.org/10.1175/jpo-d-16-0236.1
cristin:1499121
op_rights Copyright 2017 American Meteorological Society
op_doi https://doi.org/10.1175/jpo-d-16-0236.1
container_title Journal of Physical Oceanography
container_volume 47
container_issue 6
container_start_page 1473
op_container_end_page 1491
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