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The Norwegian remote sensing experiment (Norsex) in a marginal ice zonePassive and active microwave measurements from surface based, airborne, and satellite instruments were obtained together with surface observations northwest of Svalbard. Emissivities of different ice patches in the ice edge region over the spectral range from 4.9 to 94 GHz are presented. The combination of a 6.6 GHz microwave radiometer with a 14.6 GHz scatterometer demonstrates the usefulness of an active/passive system in ice classification. A variety of mesoscale features under different meteorological conditions is revealed by a 1.36 GHz synthetic aperture radar. Ice edge location by Nimbus 7 scanning multifrequency microwave radiometer is shown accurate to 10 km when the 37 GHz horizontal polarized channel is used.
Document ID
19820006693
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Farrelly, B.
(Bergen Univ. Tacoma, Wash., United States)
Johannessen, J.
(Bergen Univ. Hampton, VA, United States)
Johannessen, O. M.
(Bergen Univ. Hampton, VA, United States)
Svendson, E.
(Bergen Univ. Hampton, VA, United States)
Kloster, K.
(C. Michelson Inst.)
Horjen, I.
(Norwegian Hydrodynamic Labs.)
Campbell, W. J.
(Geological Survey)
Crawford, J.
(NASA Langley Research Center)
Harrington, R.
(NASA Langley Research Center)
Jones, L.
(NASA Langley Research Center)
Date Acquired
August 10, 2013
Publication Date
July 1, 1981
Publication Information
Publication: ESA Appl. of Remote Sensing Data on the Continental Shelf
Subject Category
Earth Resources And Remote Sensing
Accession Number
82N14566
Funding Number(s)
CONTRACT_GRANT: NATO-9.4.02-(SRG.19)
CONTRACT_GRANT: N00014-80-G-0003
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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