Modeling of anisotropic electromagnetic reflection from sea ice
Journal Article The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed, and a theoretical explanation for observed reflective anisotropy is proposed in terms of anisotropic electric flux penetration into the brine layers. The sea ice is as...
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American Geophysical Union (AGU)
1981
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ftunivutah:oai:collections.lib.utah.edu:ir_uspace/707262 2023-05-15T18:16:17+02:00 Modeling of anisotropic electromagnetic reflection from sea ice Golden, Kenneth M. Ackley, S. F. College of Science Mathematics 1981 application/pdf 1,534,122 bytes https://collections.lib.utah.edu/ark:/87278/s62r4990 eng eng American Geophysical Union (AGU) ir-main,5709 https://collections.lib.utah.edu/ark:/87278/s62r4990 (c)American Geophysical Union (AGU) Brine Anisotropy Polarization Text 1981 ftunivutah 2021-06-03T18:23:44Z Journal Article The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed, and a theoretical explanation for observed reflective anisotropy is proposed in terms of anisotropic electric flux penetration into the brine layers. The sea ice is assumed to be a stratified dielectric consisting of pure ice containing ellipsoidal conducting inclusions (brine layers) uniformly aligned with their long axes perpendicular to the preferred crystallographic c axis direction. The asymmetrical geometry of the brine layers is shown to produce an anisotropy in the complex dielectric constant of sea ice. Text Sea ice The University of Utah: J. Willard Marriott Digital Library |
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Open Polar |
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The University of Utah: J. Willard Marriott Digital Library |
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ftunivutah |
language |
English |
topic |
Brine Anisotropy Polarization |
spellingShingle |
Brine Anisotropy Polarization Golden, Kenneth M. Ackley, S. F. Modeling of anisotropic electromagnetic reflection from sea ice |
topic_facet |
Brine Anisotropy Polarization |
description |
Journal Article The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed, and a theoretical explanation for observed reflective anisotropy is proposed in terms of anisotropic electric flux penetration into the brine layers. The sea ice is assumed to be a stratified dielectric consisting of pure ice containing ellipsoidal conducting inclusions (brine layers) uniformly aligned with their long axes perpendicular to the preferred crystallographic c axis direction. The asymmetrical geometry of the brine layers is shown to produce an anisotropy in the complex dielectric constant of sea ice. |
author2 |
College of Science Mathematics |
format |
Text |
author |
Golden, Kenneth M. Ackley, S. F. |
author_facet |
Golden, Kenneth M. Ackley, S. 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 |
publisher |
American Geophysical Union (AGU) |
publishDate |
1981 |
url |
https://collections.lib.utah.edu/ark:/87278/s62r4990 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
ir-main,5709 https://collections.lib.utah.edu/ark:/87278/s62r4990 |
op_rights |
(c)American Geophysical Union (AGU) |
_version_ |
1766189833269542912 |