Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery
Sea-ice motion consists of complex non-rigid motions involving continuous, piece-wise continuous and discrete particle motion. Techniques for estimating non-rigid motion of sea ice from pairs of satellite images (generally spaced three days apart) are still in the developmental stages. For interior...
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ftdtic:ADA435632 2023-05-15T13:55:48+02:00 Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery Thomas, Mani Geiger, Cathleen Kambhamettu, Chandra COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 2004-06-27 text/html http://www.dtic.mil/docs/citations/ADA435632 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA435632 en eng http://www.dtic.mil/docs/citations/ADA435632 Approved for public release; distribution is unlimited., Availability: This document is not available from DTIC in microfiche. DTIC AND NTIS Snow Ice and Permafrost Photography Active & Passive Radar Detection & Equipment *MOTION *SYNTHETIC APERTURE RADAR *DISCONTINUITIES *SEA ICE *C BAND *SATELLITE IMAGERY ALGORITHMS ESTIMATES REMOTE DETECTION WORKSHOPS Text 2004 ftdtic 2016-02-21T13:17:01Z Sea-ice motion consists of complex non-rigid motions involving continuous, piece-wise continuous and discrete particle motion. Techniques for estimating non-rigid motion of sea ice from pairs of satellite images (generally spaced three days apart) are still in the developmental stages. For interior Arctic and Antarctic pack ice, the continuum assumption begins to fail below the 5 km scale with evidence of discontinuities already revealed in models and remote sensing products in the form of abrupt changes in magnitude and direction of the differential velocity. Using a hierarchical multi-scale phase-correlation method and profiting from known limitations of cross correlation methods, we incorporate the identification of discontinuities into our motion estimation algorithm, thereby descending below the continuum threshold to examine the phenomenon of discontinuous non-rigid sea-ice motion. Prepared in collaboration with University of Delaware, Video/Image Modeling and Synthesis Lab, Newark, DE. Pub. in Proceedings of the IEEE Workshop on Articulated and Nonrigid Motion, 2004. The original document contains color images. Text Antarc* Antarctic Arctic Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Antarctic Arctic |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Photography Active & Passive Radar Detection & Equipment *MOTION *SYNTHETIC APERTURE RADAR *DISCONTINUITIES *SEA ICE *C BAND *SATELLITE IMAGERY ALGORITHMS ESTIMATES REMOTE DETECTION WORKSHOPS |
spellingShingle |
Snow Ice and Permafrost Photography Active & Passive Radar Detection & Equipment *MOTION *SYNTHETIC APERTURE RADAR *DISCONTINUITIES *SEA ICE *C BAND *SATELLITE IMAGERY ALGORITHMS ESTIMATES REMOTE DETECTION WORKSHOPS Thomas, Mani Geiger, Cathleen Kambhamettu, Chandra Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
topic_facet |
Snow Ice and Permafrost Photography Active & Passive Radar Detection & Equipment *MOTION *SYNTHETIC APERTURE RADAR *DISCONTINUITIES *SEA ICE *C BAND *SATELLITE IMAGERY ALGORITHMS ESTIMATES REMOTE DETECTION WORKSHOPS |
description |
Sea-ice motion consists of complex non-rigid motions involving continuous, piece-wise continuous and discrete particle motion. Techniques for estimating non-rigid motion of sea ice from pairs of satellite images (generally spaced three days apart) are still in the developmental stages. For interior Arctic and Antarctic pack ice, the continuum assumption begins to fail below the 5 km scale with evidence of discontinuities already revealed in models and remote sensing products in the form of abrupt changes in magnitude and direction of the differential velocity. Using a hierarchical multi-scale phase-correlation method and profiting from known limitations of cross correlation methods, we incorporate the identification of discontinuities into our motion estimation algorithm, thereby descending below the continuum threshold to examine the phenomenon of discontinuous non-rigid sea-ice motion. Prepared in collaboration with University of Delaware, Video/Image Modeling and Synthesis Lab, Newark, DE. Pub. in Proceedings of the IEEE Workshop on Articulated and Nonrigid Motion, 2004. The original document contains color images. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Thomas, Mani Geiger, Cathleen Kambhamettu, Chandra |
author_facet |
Thomas, Mani Geiger, Cathleen Kambhamettu, Chandra |
author_sort |
Thomas, Mani |
title |
Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
title_short |
Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
title_full |
Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
title_fullStr |
Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
title_full_unstemmed |
Discontinuous Non-Rigid Motion Analysis of Sea Ice using C-Band Synthetic Aperture Radar Satellite Imagery |
title_sort |
discontinuous non-rigid motion analysis of sea ice using c-band synthetic aperture radar satellite imagery |
publishDate |
2004 |
url |
http://www.dtic.mil/docs/citations/ADA435632 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA435632 |
geographic |
Antarctic Arctic |
geographic_facet |
Antarctic Arctic |
genre |
Antarc* Antarctic Arctic Ice permafrost Sea ice |
genre_facet |
Antarc* Antarctic Arctic Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA435632 |
op_rights |
Approved for public release; distribution is unlimited., Availability: This document is not available from DTIC in microfiche. |
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1766262643040976896 |