Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature

We present a new algorithm for retrieving sea ice concentration from the AMSR-E data, the dual-polarized ratio (DPR) algorithm. The DPR algorithm is developed using vertically and horizontally polarized brightness temperatures at the same channel of 36.5 GHz. It depends on the ratio of dual-polarize...

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Published in:Journal of Oceanography
Main Authors: Zhang, Shugang, Zhao, Jinping, Frey, Karen, Su, Jie
Format: Text
Language:unknown
Published: Clark Digital Commons 2013
Subjects:
Online Access:https://commons.clarku.edu/faculty_geography/227
https://doi.org/10.1007/s10872-012-0167-z
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spelling ftclarkuniv:oai:commons.clarku.edu:faculty_geography-1226 2023-09-05T13:17:10+02:00 Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature Zhang, Shugang Zhao, Jinping Frey, Karen Su, Jie 2013-01-01T08:00:00Z https://commons.clarku.edu/faculty_geography/227 https://doi.org/10.1007/s10872-012-0167-z unknown Clark Digital Commons https://commons.clarku.edu/faculty_geography/227 doi:10.1007/s10872-012-0167-z https://doi.org/10.1007/s10872-012-0167-z Geography AMSR-E Arctic brightness temperature dual-polarized ratio algorithm ice concentration Oceanography Remote Sensing text 2013 ftclarkuniv https://doi.org/10.1007/s10872-012-0167-z 2023-08-14T06:15:24Z We present a new algorithm for retrieving sea ice concentration from the AMSR-E data, the dual-polarized ratio (DPR) algorithm. The DPR algorithm is developed using vertically and horizontally polarized brightness temperatures at the same channel of 36.5 GHz. It depends on the ratio of dual-polarized emissivity, α, which is determined empirically at about 0.92 by remotely sensed brightness temperature in winter and used for the other seasons as well. The ice concentration retrieved by the DPR is compared with those by the NT2 and ABA algorithms. Since the main difference among these algorithms takes place in marginal ice zones, 17 marginal ice zones are chosen. The retrieved ice concentrations in these zones are examined by the ice concentration obtained by the MODIS data. The mean error, root-mean-square error and mean absolute error of the DPR algorithm are relatively better than those from the other two algorithms. The results of this study illustrate that the DPR algorithm is a more accurate algorithm for retrieving sea ice concentration from the AMSR-E brightness temperature, and can be used for operational purposes. © 2013 The Oceanographic Society of Japan and Springer Japan. Text Arctic Sea ice Clark University: Clark Digital Commons Arctic Journal of Oceanography 69 2 215 227
institution Open Polar
collection Clark University: Clark Digital Commons
op_collection_id ftclarkuniv
language unknown
topic AMSR-E
Arctic
brightness temperature
dual-polarized ratio algorithm
ice concentration
Oceanography
Remote Sensing
spellingShingle AMSR-E
Arctic
brightness temperature
dual-polarized ratio algorithm
ice concentration
Oceanography
Remote Sensing
Zhang, Shugang
Zhao, Jinping
Frey, Karen
Su, Jie
Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
topic_facet AMSR-E
Arctic
brightness temperature
dual-polarized ratio algorithm
ice concentration
Oceanography
Remote Sensing
description We present a new algorithm for retrieving sea ice concentration from the AMSR-E data, the dual-polarized ratio (DPR) algorithm. The DPR algorithm is developed using vertically and horizontally polarized brightness temperatures at the same channel of 36.5 GHz. It depends on the ratio of dual-polarized emissivity, α, which is determined empirically at about 0.92 by remotely sensed brightness temperature in winter and used for the other seasons as well. The ice concentration retrieved by the DPR is compared with those by the NT2 and ABA algorithms. Since the main difference among these algorithms takes place in marginal ice zones, 17 marginal ice zones are chosen. The retrieved ice concentrations in these zones are examined by the ice concentration obtained by the MODIS data. The mean error, root-mean-square error and mean absolute error of the DPR algorithm are relatively better than those from the other two algorithms. The results of this study illustrate that the DPR algorithm is a more accurate algorithm for retrieving sea ice concentration from the AMSR-E brightness temperature, and can be used for operational purposes. © 2013 The Oceanographic Society of Japan and Springer Japan.
format Text
author Zhang, Shugang
Zhao, Jinping
Frey, Karen
Su, Jie
author_facet Zhang, Shugang
Zhao, Jinping
Frey, Karen
Su, Jie
author_sort Zhang, Shugang
title Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
title_short Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
title_full Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
title_fullStr Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
title_full_unstemmed Dual-polarized ratio algorithm for retrieving Arctic sea ice concentration from passive microwave brightness temperature
title_sort dual-polarized ratio algorithm for retrieving arctic sea ice concentration from passive microwave brightness temperature
publisher Clark Digital Commons
publishDate 2013
url https://commons.clarku.edu/faculty_geography/227
https://doi.org/10.1007/s10872-012-0167-z
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source Geography
op_relation https://commons.clarku.edu/faculty_geography/227
doi:10.1007/s10872-012-0167-z
https://doi.org/10.1007/s10872-012-0167-z
op_doi https://doi.org/10.1007/s10872-012-0167-z
container_title Journal of Oceanography
container_volume 69
container_issue 2
container_start_page 215
op_container_end_page 227
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