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A Laboratory Study of the Effect of Frost Flowers on C Band Radar Backscatter from Sea IceC band images of Arctic sea ice taken by the ERS 1 synthetic aperture radar show transitory regions of enhanced radar backscatter from young sea ice. Published field observations associate this increase with frost flower growth and the capture of blowing snow by the flowers. To investigate the first part of this phenomenon, we carried out a laboratory experiment on the response of C band radar backscatter to frost flowers growing on the surface of newly formed saline ice. The experiment took place in a 5 m by 7 m by 1.2 m deep saline water pool located in a two-story indoor refrigerated facility at the Cold Regions Research and Engineering Laboratory. Sodium chloride ice was grown in this pool at an air temperature of -28 C. The frost flowers first appeared on the ice surface as dendrites and then changed to needles as the ice sheet grew thicker and the surface temperatures became colder. The frost flowers reached to a height of 10-15 mm, and beneath each cluster of frost flowers a slush layer formed to a thickness of approximately 4 mm. Far-field radar measurements of the backscatter from the ice were made at incident angles from 20 to 40 deg and at approximately 6-hour intervals throughout the 3-day period of the experiment. A backscatter minimum occurred early in the flower growth at the time coincident with an abrupt doubling in the ice surface salinity. Once the full flower coverage was achieved, we removed first the crystal flowers and then the slush layer from the ice surface. The results for these cases show that the crystals have little impact on the backscatter, while the underlying slush patches yield a backscatter increase of 3-5 dB over that of bare ice. The laboratory results suggest that this relative backscatter increase of approximately 5 dB can be used as an index to mark the full area coverage of frost flowers.
Document ID
19980227533
Acquisition Source
Jet Propulsion Laboratory
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Nghiem, S. V.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Martin, S.
(Washington Univ. Seattle, WA United States)
Perovich, D. K.
(Army Cold Regions Research and Engineering Lab. Hanover, NH United States)
Kwok, R.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Drucker, R.
(Washington Univ. Seattle, WA United States)
Gow, A. J.
(Army Cold Regions Research and Engineering Lab. Hanover, NH United States)
Date Acquired
August 18, 2013
Publication Date
February 15, 1997
Publication Information
Publication: Journal of Geophysical Research
Publisher: American Geophysical Union
Volume: 102
Issue: C2
ISSN: 0148-0227
Subject Category
Communications And Radar
Report/Patent Number
Paper-96JC03208
Funding Number(s)
CONTRACT_GRANT: N00014-95-MP-3019
CONTRACT_GRANT: N00014-95-MP-3002
CONTRACT_GRANT: N00014-90-J-0161
Distribution Limits
Public
Copyright
Other

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