Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data

Abstract The limitations of current and immediate future single-frequency, single-polarization, space-borne SARs for winter sea-ice mapping are quantitatively examined, and improvements are suggested by combining frequencies and polarizations. Ice-type maps are generated using multi-channel, air-bor...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Rignot, Eric, Drinkwater, Mark R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1994
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000003774
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003774
id crcambridgeupr:10.1017/s0022143000003774
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000003774 2024-09-15T17:58:49+00:00 Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data Rignot, Eric Drinkwater, Mark R. 1994 http://dx.doi.org/10.1017/s0022143000003774 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003774 en eng Cambridge University Press (CUP) Journal of Glaciology volume 40, issue 134, page 31-45 ISSN 0022-1430 1727-5652 journal-article 1994 crcambridgeupr https://doi.org/10.1017/s0022143000003774 2024-07-24T04:04:15Z Abstract The limitations of current and immediate future single-frequency, single-polarization, space-borne SARs for winter sea-ice mapping are quantitatively examined, and improvements are suggested by combining frequencies and polarizations. Ice-type maps are generated using multi-channel, air-borne SAR observations of winter sea ice in the Beaufort Sea to identify six ice conditions: (1) multi-year sea ice; (2) compressed first-year ice; (3) first-year rubble and ridges; (4) first-year rough ice; (5) first-year smooth ice; and (6) first-year thin ice. At a single polarization, C- (λ = 5.6 cm) and L- (λ = 24 cm) band frequencies yield a classification accuracy of 67 and 71%, because C-band confuses multi-year ice and compressed, rough, thick first-year ice surrounding multi-year ice floes, and L-band confuses multi-year ice and deformed first-year ice. Combining C- and L-band improves classification accuracy by 20%. Adding a second polarization at one frequency only improves classification accuracy by 10–14% and separates thin ice and calm open water. Under similar winter-ice conditions, ERS-1 ( C vv ) and Radarsat ( C HH ) would overestimate the multi-year ice fraction by 15% but correctly map the spatial variability of ice thickness; J-ERS-1 ( L HH ) would perform poorly;and J-ERS-1 combined with ERS-1 or Radarsat would yield reliable estimates of the old, thick, first-year and thin-ice fractions, and of the spatial distribution of ridges. With two polarizations, future single-frequency space-borne SARs could improve our current capability to discriminate thinner ice types. Article in Journal/Newspaper Beaufort Sea Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 40 134 31 45
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The limitations of current and immediate future single-frequency, single-polarization, space-borne SARs for winter sea-ice mapping are quantitatively examined, and improvements are suggested by combining frequencies and polarizations. Ice-type maps are generated using multi-channel, air-borne SAR observations of winter sea ice in the Beaufort Sea to identify six ice conditions: (1) multi-year sea ice; (2) compressed first-year ice; (3) first-year rubble and ridges; (4) first-year rough ice; (5) first-year smooth ice; and (6) first-year thin ice. At a single polarization, C- (λ = 5.6 cm) and L- (λ = 24 cm) band frequencies yield a classification accuracy of 67 and 71%, because C-band confuses multi-year ice and compressed, rough, thick first-year ice surrounding multi-year ice floes, and L-band confuses multi-year ice and deformed first-year ice. Combining C- and L-band improves classification accuracy by 20%. Adding a second polarization at one frequency only improves classification accuracy by 10–14% and separates thin ice and calm open water. Under similar winter-ice conditions, ERS-1 ( C vv ) and Radarsat ( C HH ) would overestimate the multi-year ice fraction by 15% but correctly map the spatial variability of ice thickness; J-ERS-1 ( L HH ) would perform poorly;and J-ERS-1 combined with ERS-1 or Radarsat would yield reliable estimates of the old, thick, first-year and thin-ice fractions, and of the spatial distribution of ridges. With two polarizations, future single-frequency space-borne SARs could improve our current capability to discriminate thinner ice types.
format Article in Journal/Newspaper
author Rignot, Eric
Drinkwater, Mark R.
spellingShingle Rignot, Eric
Drinkwater, Mark R.
Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
author_facet Rignot, Eric
Drinkwater, Mark R.
author_sort Rignot, Eric
title Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
title_short Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
title_full Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
title_fullStr Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
title_full_unstemmed Winter Sea-ice mapping from multi-parameter synthetic-aperture radar data
title_sort winter sea-ice mapping from multi-parameter synthetic-aperture radar data
publisher Cambridge University Press (CUP)
publishDate 1994
url http://dx.doi.org/10.1017/s0022143000003774
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003774
genre Beaufort Sea
Journal of Glaciology
Sea ice
genre_facet Beaufort Sea
Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 40, issue 134, page 31-45
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000003774
container_title Journal of Glaciology
container_volume 40
container_issue 134
container_start_page 31
op_container_end_page 45
_version_ 1810435790448099328