Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data

3D realistic sea surface imaging from 3D dual-sensor towed streamer data is presented. The technique is based on separating data acquired by collocated dual-sensors into up-going and down-going wavefields. Subsequently, these wavefields are extrapolated upwards in order to image the sea surface. Thi...

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Main Authors: Okwudili C. Orji, Walter Söllner, Leiv-J. Gelius
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2013/387175
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spelling doaj-97991a63295a47768cc7dd5c7f8af4252020-11-24T22:31:45ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682013-01-01201310.1155/2013/387175387175Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer DataOkwudili C. Orji0Walter Söllner1Leiv-J. Gelius2Petroleum Geo-Services, Lysaker, 1325 Oslo, NorwayPetroleum Geo-Services, Lysaker, 1325 Oslo, NorwayUniversity of Oslo, 0316 Oslo, Norway3D realistic sea surface imaging from 3D dual-sensor towed streamer data is presented. The technique is based on separating data acquired by collocated dual-sensors into up-going and down-going wavefields. Subsequently, these wavefields are extrapolated upwards in order to image the sea surface. This approach has previously been demonstrated using 2D data examples. Here, the focus is on 3D data. Controlled 3D data based on the Kirchhoff-Helmholtz algorithm is generated, and the 3D sea surface imaging technique is applied. For coarsely spaced streamers from 3D field data, the technique is applied streamerwise (i.e., 2D wavefield separation, extrapolation, and imaging). In the latter case, the resulting sea surface profiles corresponding to each time frame are interpolated to demonstrate that the main sea surface characteristics are preserved, and artefacts due to 2D processing of 3D data are mainly limited to areas corresponding to large angles of incidence. Time-varying sea surfaces from two different 3D field data are imaged. The data examples were acquired under different weather conditions. The imaged sea surfaces show realistic wave heights, and their spectra suggest plausible speeds and directions.http://dx.doi.org/10.1155/2013/387175
collection DOAJ
language English
format Article
sources DOAJ
author Okwudili C. Orji
Walter Söllner
Leiv-J. Gelius
spellingShingle Okwudili C. Orji
Walter Söllner
Leiv-J. Gelius
Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
International Journal of Geophysics
author_facet Okwudili C. Orji
Walter Söllner
Leiv-J. Gelius
author_sort Okwudili C. Orji
title Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
title_short Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
title_full Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
title_fullStr Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
title_full_unstemmed Imaging 3D Sea Surfaces from 3D Dual-Sensor Towed Streamer Data
title_sort imaging 3d sea surfaces from 3d dual-sensor towed streamer data
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2013-01-01
description 3D realistic sea surface imaging from 3D dual-sensor towed streamer data is presented. The technique is based on separating data acquired by collocated dual-sensors into up-going and down-going wavefields. Subsequently, these wavefields are extrapolated upwards in order to image the sea surface. This approach has previously been demonstrated using 2D data examples. Here, the focus is on 3D data. Controlled 3D data based on the Kirchhoff-Helmholtz algorithm is generated, and the 3D sea surface imaging technique is applied. For coarsely spaced streamers from 3D field data, the technique is applied streamerwise (i.e., 2D wavefield separation, extrapolation, and imaging). In the latter case, the resulting sea surface profiles corresponding to each time frame are interpolated to demonstrate that the main sea surface characteristics are preserved, and artefacts due to 2D processing of 3D data are mainly limited to areas corresponding to large angles of incidence. Time-varying sea surfaces from two different 3D field data are imaged. The data examples were acquired under different weather conditions. The imaged sea surfaces show realistic wave heights, and their spectra suggest plausible speeds and directions.
url http://dx.doi.org/10.1155/2013/387175
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AT leivjgelius imaging3dseasurfacesfrom3ddualsensortowedstreamerdata
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