3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data

Multi-frequency C and L bands in the TOPSAR data have been utilized to reconstruct three-dimensional (3-D) bathymetry pattern. The main objective of this study is to utilize fuzzy arithmetic to reduce the errors arising from speckle in synthetic aperture radar (SAR) data when constructing ocean bath...

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Main Authors: Marghany, Maged Mahmoud, Cracknell, Arthur P., Hashim, Mazlan
Format: Article
Published: Taylor & Francis Online 2010
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Online Access:http://eprints.utm.my/id/eprint/22782/
http://dx.doi.org/10.1080/17538940903477406
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Institution: Universiti Teknologi Malaysia
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spelling my.utm.227822018-03-12T03:16:57Z http://eprints.utm.my/id/eprint/22782/ 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data Marghany, Maged Mahmoud Cracknell, Arthur P. Hashim, Mazlan HD Industries. Land use. Labor Multi-frequency C and L bands in the TOPSAR data have been utilized to reconstruct three-dimensional (3-D) bathymetry pattern. The main objective of this study is to utilize fuzzy arithmetic to reduce the errors arising from speckle in synthetic aperture radar (SAR) data when constructing ocean bathymetry from polarized SAR data. In doing so, two 3-D surface models, the Volterra algorithm and a fuzzy B-spline (FBS) algorithm, which construct a global topological structure between the data points, were used to support an approximation to the real surface. Volterra algorithm was used to express the non-linearity of TOPSAR data intensity gradient based on the action balance equation (ABC). In this context, a first-order kernel of Volterra algorithm was used to express ABC equation. The inverse of Volterra algorithm then performed to simulate 2-D current velocities from CVV and LHH band. Furthermore, the 2-D continuity equation then used to estimate the water depth. In order to reconstruct 3-D bathymetry pattern, the FBS has been performed to water depth information which was estimated from 2-D continuity equation. The best reconstruction of coastal bathymetry of the test site in Kuala Terengganu, Malaysia, was obtained with polarized L and C bands SAR acquired with HH and VV polarizations, respectively. With 10 m spatial resolution of TOPSAR data, bias of –0.004 m, the standard error mean of 0.023 m, r 2 value of 0.95, and 90% confidence intervals in depth determination was obtained with LHH band. Taylor & Francis Online 2010-06 Article PeerReviewed Marghany, Maged Mahmoud and Cracknell, Arthur P. and Hashim, Mazlan (2010) 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data. International Journal of Digital Earth, 3 (2). 187 - 206. ISSN 17538947 http://dx.doi.org/10.1080/17538940903477406 10.1080/17538940903477406
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
topic HD Industries. Land use. Labor
spellingShingle HD Industries. Land use. Labor
Marghany, Maged Mahmoud
Cracknell, Arthur P.
Hashim, Mazlan
3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
description Multi-frequency C and L bands in the TOPSAR data have been utilized to reconstruct three-dimensional (3-D) bathymetry pattern. The main objective of this study is to utilize fuzzy arithmetic to reduce the errors arising from speckle in synthetic aperture radar (SAR) data when constructing ocean bathymetry from polarized SAR data. In doing so, two 3-D surface models, the Volterra algorithm and a fuzzy B-spline (FBS) algorithm, which construct a global topological structure between the data points, were used to support an approximation to the real surface. Volterra algorithm was used to express the non-linearity of TOPSAR data intensity gradient based on the action balance equation (ABC). In this context, a first-order kernel of Volterra algorithm was used to express ABC equation. The inverse of Volterra algorithm then performed to simulate 2-D current velocities from CVV and LHH band. Furthermore, the 2-D continuity equation then used to estimate the water depth. In order to reconstruct 3-D bathymetry pattern, the FBS has been performed to water depth information which was estimated from 2-D continuity equation. The best reconstruction of coastal bathymetry of the test site in Kuala Terengganu, Malaysia, was obtained with polarized L and C bands SAR acquired with HH and VV polarizations, respectively. With 10 m spatial resolution of TOPSAR data, bias of –0.004 m, the standard error mean of 0.023 m, r 2 value of 0.95, and 90% confidence intervals in depth determination was obtained with LHH band.
format Article
author Marghany, Maged Mahmoud
Cracknell, Arthur P.
Hashim, Mazlan
author_facet Marghany, Maged Mahmoud
Cracknell, Arthur P.
Hashim, Mazlan
author_sort Marghany, Maged Mahmoud
title 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
title_short 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
title_full 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
title_fullStr 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
title_full_unstemmed 3-D visualizations of coastal bathymetry by utilization of airborne TOPSAR polarized data
title_sort 3-d visualizations of coastal bathymetry by utilization of airborne topsar polarized data
publisher Taylor & Francis Online
publishDate 2010
url http://eprints.utm.my/id/eprint/22782/
http://dx.doi.org/10.1080/17538940903477406
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