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...

Full description

Bibliographic Details
Main Author: Brock, Billy C.
Other Authors: United States. Department of Energy.
Format: Report
Language:English
Published: Sandia National Laboratories 2010
Subjects:
Online Access:https://doi.org/10.2172/989382
https://digital.library.unt.edu/ark:/67531/metadc1013276/
id ftunivnotexas:info:ark/67531/metadc1013276
record_format openpolar
spelling 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