Modeling of Anisotropic Electromagnetic Reflection from Sea Ice
The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed. The sea ice is considered to be a stratified, inhomogeneous, anisotropic dielectric consisting of pure ice containing ordered arrays of conducting inclusions (brine layers). Below the...
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ftdtic:ADA094620 2023-05-15T16:37:22+02:00 Modeling of Anisotropic Electromagnetic Reflection from Sea Ice Golden,Kenneth M Ackley,Stephen F COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1980-10 text/html http://www.dtic.mil/docs/citations/ADA094620 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA094620 en eng http://www.dtic.mil/docs/citations/ADA094620 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Radiofrequency Wave Propagation *RADAR REFLECTIONS *SEA ICE MATHEMATICAL MODELS LAYERS ANISOTROPY BRINES Text 1980 ftdtic 2016-02-20T19:23:08Z The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed. The sea ice is considered to be a stratified, inhomogeneous, anisotropic dielectric consisting of pure ice containing ordered arrays of conducting inclusions (brine layers). Below the transition zone, the ice is assumed to have constant azimuthal c-axis orientation within the horizontal plane, so that the orientation of brine layers is uniform. The brine layers are also assumed to become increasingly well-defined with depth, since adjacent brine inclusions tend to fuse together with increasing temperature. A theoretical explanation for observed reflective anisotropy is proposed in terms of anisotropic electric flux penetration into the brine layers. Penetration anisotropy and brine layer geometry are linked to anisotropy in the complex dielectric constant of sea ice. In order to illustrate the above effects we present a numerical method of approximating the reflected power of a plane wave pulse incident on a slab of sea ice. Mixture dielectric constants are calculated for two polarizations of the incident wave: (1) the electric field parallel to the c-axis direction, and (2) the electric field perpendicular to the c-axis direction. These dielectric constants are then used to calculate power reflection coefficients for the two polarizations. Significant bottom reflection (R approximates 0.08) occurs when the polarization is parallel to the c-axis. However, when the polarization is perpendicular to the c-axis, the return may be almost completely extinguished (R less than 0.001). (Author) Text Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Radiofrequency Wave Propagation *RADAR REFLECTIONS *SEA ICE MATHEMATICAL MODELS LAYERS ANISOTROPY BRINES |
spellingShingle |
Snow Ice and Permafrost Radiofrequency Wave Propagation *RADAR REFLECTIONS *SEA ICE MATHEMATICAL MODELS LAYERS ANISOTROPY BRINES Golden,Kenneth M Ackley,Stephen F Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
topic_facet |
Snow Ice and Permafrost Radiofrequency Wave Propagation *RADAR REFLECTIONS *SEA ICE MATHEMATICAL MODELS LAYERS ANISOTROPY BRINES |
description |
The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed. The sea ice is considered to be a stratified, inhomogeneous, anisotropic dielectric consisting of pure ice containing ordered arrays of conducting inclusions (brine layers). Below the transition zone, the ice is assumed to have constant azimuthal c-axis orientation within the horizontal plane, so that the orientation of brine layers is uniform. The brine layers are also assumed to become increasingly well-defined with depth, since adjacent brine inclusions tend to fuse together with increasing temperature. A theoretical explanation for observed reflective anisotropy is proposed in terms of anisotropic electric flux penetration into the brine layers. Penetration anisotropy and brine layer geometry are linked to anisotropy in the complex dielectric constant of sea ice. In order to illustrate the above effects we present a numerical method of approximating the reflected power of a plane wave pulse incident on a slab of sea ice. Mixture dielectric constants are calculated for two polarizations of the incident wave: (1) the electric field parallel to the c-axis direction, and (2) the electric field perpendicular to the c-axis direction. These dielectric constants are then used to calculate power reflection coefficients for the two polarizations. Significant bottom reflection (R approximates 0.08) occurs when the polarization is parallel to the c-axis. However, when the polarization is perpendicular to the c-axis, the return may be almost completely extinguished (R less than 0.001). (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Golden,Kenneth M Ackley,Stephen F |
author_facet |
Golden,Kenneth M Ackley,Stephen F |
author_sort |
Golden,Kenneth M |
title |
Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
title_short |
Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
title_full |
Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
title_fullStr |
Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
title_full_unstemmed |
Modeling of Anisotropic Electromagnetic Reflection from Sea Ice |
title_sort |
modeling of anisotropic electromagnetic reflection from sea ice |
publishDate |
1980 |
url |
http://www.dtic.mil/docs/citations/ADA094620 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA094620 |
genre |
Ice permafrost Sea ice |
genre_facet |
Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA094620 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027666514771968 |