Microwave signatures of first-year and multiyear sea ice

A combination of remote sensing from an aircraft and simultaneous surface measurements have confirmed the feasibility of identifying old and new sea ice according to its emission of thermal radiation at wavelengths between 0.3 and 3 cm. Emissivity of first-year thick ice with a surface temperature o...

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Main Authors: Nordberg, P., Schmugge, T. J., Wilheit, T. T., Campbell, W. J., Gloersen, P.
Format: Other/Unknown Material
Language:unknown
Published: 1972
Subjects:
Online Access:http://hdl.handle.net/2060/19720022699
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author Nordberg, P.
Schmugge, T. J.
Wilheit, T. T.
Campbell, W. J.
Gloersen, P.
author_facet Nordberg, P.
Schmugge, T. J.
Wilheit, T. T.
Campbell, W. J.
Gloersen, P.
author_sort Nordberg, P.
collection NASA Technical Reports Server (NTRS)
description A combination of remote sensing from an aircraft and simultaneous surface measurements have confirmed the feasibility of identifying old and new sea ice according to its emission of thermal radiation at wavelengths between 0.3 and 3 cm. Emissivity of first-year thick ice with a surface temperature of about 260 K is 0.95 or greater for wavelengths between 0.81 and 11 cm; the emissivity of multiyear ice is 0.8 at 0.81 cm and 0.95 at 11 cm, increasing monotonically in this wave length interval. The ease with which multiyear ice can be distinguished from first-year ice using a passive microwave radiometer is demonstrated by comparing mosaics prepared both from photographs and images of 1.55 cm radiation.
format Other/Unknown Material
genre Sea ice
genre_facet Sea ice
id ftnasantrs:oai:casi.ntrs.nasa.gov:19720022699
institution Open Polar
language unknown
op_collection_id ftnasantrs
op_coverage Unclassified, Unlimited, Publicly available
op_relation Document ID: 19720022699
Accession ID: 72N30349
http://hdl.handle.net/2060/19720022699
op_rights No Copyright
op_source CASI
publishDate 1972
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19720022699 2025-01-17T00:43:43+00:00 Microwave signatures of first-year and multiyear sea ice Nordberg, P. Schmugge, T. J. Wilheit, T. T. Campbell, W. J. Gloersen, P. Unclassified, Unlimited, Publicly available Aug 1, 1972 application/pdf http://hdl.handle.net/2060/19720022699 unknown Document ID: 19720022699 Accession ID: 72N30349 http://hdl.handle.net/2060/19720022699 No Copyright CASI GEOPHYSICS NASA-TM-X-66006 X-652-72-312 1972 ftnasantrs 2019-07-21T11:37:41Z A combination of remote sensing from an aircraft and simultaneous surface measurements have confirmed the feasibility of identifying old and new sea ice according to its emission of thermal radiation at wavelengths between 0.3 and 3 cm. Emissivity of first-year thick ice with a surface temperature of about 260 K is 0.95 or greater for wavelengths between 0.81 and 11 cm; the emissivity of multiyear ice is 0.8 at 0.81 cm and 0.95 at 11 cm, increasing monotonically in this wave length interval. The ease with which multiyear ice can be distinguished from first-year ice using a passive microwave radiometer is demonstrated by comparing mosaics prepared both from photographs and images of 1.55 cm radiation. Other/Unknown Material Sea ice NASA Technical Reports Server (NTRS)
spellingShingle GEOPHYSICS
Nordberg, P.
Schmugge, T. J.
Wilheit, T. T.
Campbell, W. J.
Gloersen, P.
Microwave signatures of first-year and multiyear sea ice
title Microwave signatures of first-year and multiyear sea ice
title_full Microwave signatures of first-year and multiyear sea ice
title_fullStr Microwave signatures of first-year and multiyear sea ice
title_full_unstemmed Microwave signatures of first-year and multiyear sea ice
title_short Microwave signatures of first-year and multiyear sea ice
title_sort microwave signatures of first-year and multiyear sea ice
topic GEOPHYSICS
topic_facet GEOPHYSICS
url http://hdl.handle.net/2060/19720022699