On the detection of crevasses in glacial ice with synthetic-aperture radar.
The intent of this study is to provide an analysis of the scattering from a crevasse in Antarctic ice, utilizing a physics-based model for the scattering process. Of primary interest is a crevasse covered with a snow bridge, which makes the crevasse undetectable in visible-light images. It is demons...
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ftunivnotexas:info:ark/67531/metadc1013276 2023-05-15T14:03:28+02:00 On the detection of crevasses in glacial ice with synthetic-aperture radar. Brock, Billy C. United States. Department of Energy. 2010-02-01 174 p. Text https://doi.org/10.2172/989382 https://digital.library.unt.edu/ark:/67531/metadc1013276/ English eng Sandia National Laboratories rep-no: SAND2010-0363 grantno: AC04-94AL85000 doi:10.2172/989382 osti: 989382 https://digital.library.unt.edu/ark:/67531/metadc1013276/ ark: ark:/67531/metadc1013276 Dielectric Materials 36 Materials Science Snow Radar Synthetic Aperture Radar-Image Quality Viability Glaciers-Forecasting Fractals Detection Glaciers Scattering Glaciers-Forecasting Permittivity Report 2010 ftunivnotexas https://doi.org/10.2172/989382 2017-10-28T22:08:06Z The intent of this study is to provide an analysis of the scattering from a crevasse in Antarctic ice, utilizing a physics-based model for the scattering process. Of primary interest is a crevasse covered with a snow bridge, which makes the crevasse undetectable in visible-light images. It is demonstrated that a crevasse covered with a snow bridge can be visible in synthetic-aperture-radar (SAR) images. The model of the crevasse and snow bridge incorporates a complex dielectric permittivity model for dry snow and ice that takes into account the density profile of the glacier. The surface structure is based on a fractal model that can produce sastrugi-like features found on the surface of Antarctic glaciers. Simulated phase histories, computed with the Shooting and Bouncing Ray (SBR) method, are processed into SAR images. The viability of the SBR method for predicting scattering from a crevasse covered with a snow bridge is demonstrated. Some suggestions for improving the model are given. Report Antarc* Antarctic University of North Texas: UNT Digital Library Antarctic Sastrugi ENVELOPE(163.683,163.683,-74.617,-74.617) |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Dielectric Materials 36 Materials Science Snow Radar Synthetic Aperture Radar-Image Quality Viability Glaciers-Forecasting Fractals Detection Glaciers Scattering Glaciers-Forecasting Permittivity |
spellingShingle |
Dielectric Materials 36 Materials Science Snow Radar Synthetic Aperture Radar-Image Quality Viability Glaciers-Forecasting Fractals Detection Glaciers Scattering Glaciers-Forecasting Permittivity Brock, Billy C. On the detection of crevasses in glacial ice with synthetic-aperture radar. |
topic_facet |
Dielectric Materials 36 Materials Science Snow Radar Synthetic Aperture Radar-Image Quality Viability Glaciers-Forecasting Fractals Detection Glaciers Scattering Glaciers-Forecasting Permittivity |
description |
The intent of this study is to provide an analysis of the scattering from a crevasse in Antarctic ice, utilizing a physics-based model for the scattering process. Of primary interest is a crevasse covered with a snow bridge, which makes the crevasse undetectable in visible-light images. It is demonstrated that a crevasse covered with a snow bridge can be visible in synthetic-aperture-radar (SAR) images. The model of the crevasse and snow bridge incorporates a complex dielectric permittivity model for dry snow and ice that takes into account the density profile of the glacier. The surface structure is based on a fractal model that can produce sastrugi-like features found on the surface of Antarctic glaciers. Simulated phase histories, computed with the Shooting and Bouncing Ray (SBR) method, are processed into SAR images. The viability of the SBR method for predicting scattering from a crevasse covered with a snow bridge is demonstrated. Some suggestions for improving the model are given. |
author2 |
United States. Department of Energy. |
format |
Report |
author |
Brock, Billy C. |
author_facet |
Brock, Billy C. |
author_sort |
Brock, Billy C. |
title |
On the detection of crevasses in glacial ice with synthetic-aperture radar. |
title_short |
On the detection of crevasses in glacial ice with synthetic-aperture radar. |
title_full |
On the detection of crevasses in glacial ice with synthetic-aperture radar. |
title_fullStr |
On the detection of crevasses in glacial ice with synthetic-aperture radar. |
title_full_unstemmed |
On the detection of crevasses in glacial ice with synthetic-aperture radar. |
title_sort |
on the detection of crevasses in glacial ice with synthetic-aperture radar. |
publisher |
Sandia National Laboratories |
publishDate |
2010 |
url |
https://doi.org/10.2172/989382 https://digital.library.unt.edu/ark:/67531/metadc1013276/ |
long_lat |
ENVELOPE(163.683,163.683,-74.617,-74.617) |
geographic |
Antarctic Sastrugi |
geographic_facet |
Antarctic Sastrugi |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
rep-no: SAND2010-0363 grantno: AC04-94AL85000 doi:10.2172/989382 osti: 989382 https://digital.library.unt.edu/ark:/67531/metadc1013276/ ark: ark:/67531/metadc1013276 |
op_doi |
https://doi.org/10.2172/989382 |
_version_ |
1766274125388578816 |