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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Main Authors: Golden, Kenneth M., Ackley, S. F.
Other Authors: College of Science, Mathematics
Format: Text
Language:English
Published: American Geophysical Union (AGU) 1981
Subjects:
Online Access:https://collections.lib.utah.edu/ark:/87278/s62r4990
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spelling 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
institution Open Polar
collection The University of Utah: J. Willard Marriott Digital Library
op_collection_id 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