Electromagnetic and physical properties of sea ice formed in the presence of wave action

Estimating the magnitude of brine flux to the upper ocean requires an ability to assess the dynamics of the formation of sea ice in a region. Brine storage and rate of expulsion is determined by the environmental conditions under which the sea ice forms. In this paper, the physical and electromagnet...

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Main Authors: Onstott, Robert G., Gogineni, Sivaprasad, Gow, Anthony J., Grenfell, Thomas C., Jezek, Kenneth C., Perovich, Donald K., Swift, C. T.
Format: Article in Journal/Newspaper
Language:English
Published: IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC 2007
Subjects:
Online Access:http://hdl.handle.net/1808/1320
id ftunivkansas:oai:kuscholarworks.ku.edu:1808/1320
record_format openpolar
spelling ftunivkansas:oai:kuscholarworks.ku.edu:1808/1320 2023-05-15T18:16:25+02:00 Electromagnetic and physical properties of sea ice formed in the presence of wave action Onstott, Robert G. Gogineni, Sivaprasad Gow, Anthony J. Grenfell, Thomas C. Jezek, Kenneth C. Perovich, Donald K. Swift, C. T. 2007-04-09T23:45:21Z http://hdl.handle.net/1808/1320 en_US eng IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC Onstott, RG; Gogineni, P; Gow, AJ; Grenfell, TC; Jezek, KC; Perovich, DK; Swift, CT. Electromagnetic and physical properties of sea ice formed in the presence of wave action. IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING. September 1998. 36(5, 2) 1764-1783 http://hdl.handle.net/1808/1320 openAccess Backscatter Electromagnetics Emissions Pancake ice Sea ice Article 2007 ftunivkansas 2022-08-26T13:09:01Z Estimating the magnitude of brine flux to the upper ocean requires an ability to assess the dynamics of the formation of sea ice in a region. Brine storage and rate of expulsion is determined by the environmental conditions under which the sea ice forms. In this paper, the physical and electromagnetic properties of sea ice, formed under wave-agitated conditions, are studied and compared with results obtained from ice formed under quiescent conditions. Wave agitation is known to have a profound effect on the air-ice interface and internal ice structure. A variety of sensors, both active and passive, optical and microwave, were used to perform this characterization. Measured electromagnetic parameters included radar backscatter, microwave emission, and spectral albedo in the visible and infrared. Measured physical properties included ice structure, brine and temperature distribution, profiles of the vertical height of the air-ice interface, and ice formation processes. Results showed that emission, backscatter, and albedo all take different signature paths during the transformation from saline water to young sea ice and that the paths depend on sea surface state during ice formation. Article in Journal/Newspaper Sea ice The University of Kansas: KU ScholarWorks Pancake ENVELOPE(-55.815,-55.815,52.600,52.600)
institution Open Polar
collection The University of Kansas: KU ScholarWorks
op_collection_id ftunivkansas
language English
topic Backscatter
Electromagnetics
Emissions
Pancake ice
Sea ice
spellingShingle Backscatter
Electromagnetics
Emissions
Pancake ice
Sea ice
Onstott, Robert G.
Gogineni, Sivaprasad
Gow, Anthony J.
Grenfell, Thomas C.
Jezek, Kenneth C.
Perovich, Donald K.
Swift, C. T.
Electromagnetic and physical properties of sea ice formed in the presence of wave action
topic_facet Backscatter
Electromagnetics
Emissions
Pancake ice
Sea ice
description Estimating the magnitude of brine flux to the upper ocean requires an ability to assess the dynamics of the formation of sea ice in a region. Brine storage and rate of expulsion is determined by the environmental conditions under which the sea ice forms. In this paper, the physical and electromagnetic properties of sea ice, formed under wave-agitated conditions, are studied and compared with results obtained from ice formed under quiescent conditions. Wave agitation is known to have a profound effect on the air-ice interface and internal ice structure. A variety of sensors, both active and passive, optical and microwave, were used to perform this characterization. Measured electromagnetic parameters included radar backscatter, microwave emission, and spectral albedo in the visible and infrared. Measured physical properties included ice structure, brine and temperature distribution, profiles of the vertical height of the air-ice interface, and ice formation processes. Results showed that emission, backscatter, and albedo all take different signature paths during the transformation from saline water to young sea ice and that the paths depend on sea surface state during ice formation.
format Article in Journal/Newspaper
author Onstott, Robert G.
Gogineni, Sivaprasad
Gow, Anthony J.
Grenfell, Thomas C.
Jezek, Kenneth C.
Perovich, Donald K.
Swift, C. T.
author_facet Onstott, Robert G.
Gogineni, Sivaprasad
Gow, Anthony J.
Grenfell, Thomas C.
Jezek, Kenneth C.
Perovich, Donald K.
Swift, C. T.
author_sort Onstott, Robert G.
title Electromagnetic and physical properties of sea ice formed in the presence of wave action
title_short Electromagnetic and physical properties of sea ice formed in the presence of wave action
title_full Electromagnetic and physical properties of sea ice formed in the presence of wave action
title_fullStr Electromagnetic and physical properties of sea ice formed in the presence of wave action
title_full_unstemmed Electromagnetic and physical properties of sea ice formed in the presence of wave action
title_sort electromagnetic and physical properties of sea ice formed in the presence of wave action
publisher IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
publishDate 2007
url http://hdl.handle.net/1808/1320
long_lat ENVELOPE(-55.815,-55.815,52.600,52.600)
geographic Pancake
geographic_facet Pancake
genre Sea ice
genre_facet Sea ice
op_relation Onstott, RG; Gogineni, P; Gow, AJ; Grenfell, TC; Jezek, KC; Perovich, DK; Swift, CT. Electromagnetic and physical properties of sea ice formed in the presence of wave action. IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING. September 1998. 36(5, 2) 1764-1783
http://hdl.handle.net/1808/1320
op_rights openAccess
_version_ 1766190007900438528