DocumentCode
2946776
Title
Interpretation of radar returns from sea ice
Author
Byrd, Robert C.
Author_Institution
Univ. of Alaska, Fairbanks, Alaska, USA
fYear
1971
fDate
21-24 Sept. 1971
Firstpage
349
Lastpage
352
Abstract
The heterogeneous nature of the sea ice surface with respect to topography and reflectivity characteristics poses serious problems in interpreting radar returns to the precision needed for modern transportation over the polar ice pack. The physical properties of sea ice are discussed. A swept frequency technique is used to determine the electromagnetic properties of 
salinity sea ice in the frequency band from 26.5 to 40.0 GHz. Lack of influence by liquid brine is noted in the real part of the complex permittivity at temperatures below 
C; a marked change in dielectric loss is noted with change in the orientation of the liquid brine inclusions in sea ice with respect to the millimeter wave electric field
salinity sea ice in the frequency band from 26.5 to 40.0 GHz. Lack of influence by liquid brine is noted in the real part of the complex permittivity at temperatures below C; a marked change in dielectric loss is noted with change in the orientation of the liquid brine inclusions in sea ice with respect to the millimeter wave electric fieldKeywords
Dielectric losses; Frequency; Ice surface; Ocean temperature; Sea ice; Sea surface; Solids; Surface topography; Temperature dependence; Temperature distribution;
fLanguage
English
Publisher
ieee
Conference_Titel
Engineering in the Ocean Environment, IEEE 1971 Conference on
Conference_Location
San Diego, CA, USA
Type
conf
DOI
10.1109/OCEANS.1971.1161009
Filename
1161009
Link To Document