Sea ice mapping method for SeaWinds

A sea ice mapping algorithm for SeaWinds is developed that incorporates statistical and spatial a priori information in a modified maximum a posteriori (MAP) framework. Spatial a priori data are incorporated in the loss terms of a Bayes risk formulation. Conditional distributions and priors for sea...

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Main Authors: Long, David G., Anderson, Hyrum S.
Format: Text
Language:English
Published: BYU ScholarsArchive 2005
Subjects:
Online Access:https://scholarsarchive.byu.edu/facpub/391
https://scholarsarchive.byu.edu/context/facpub/article/1390/viewcontent/IR_CISOPTR_713.pdf
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spelling ftbrighamyoung:oai:scholarsarchive.byu.edu:facpub-1390 2023-07-23T04:19:50+02:00 Sea ice mapping method for SeaWinds Long, David G. Anderson, Hyrum S. 2005-03-01T08:00:00Z application/pdf https://scholarsarchive.byu.edu/facpub/391 https://scholarsarchive.byu.edu/context/facpub/article/1390/viewcontent/IR_CISOPTR_713.pdf English eng BYU ScholarsArchive https://scholarsarchive.byu.edu/facpub/391 https://scholarsarchive.byu.edu/context/facpub/article/1390/viewcontent/IR_CISOPTR_713.pdf Faculty Publications Bayes methods geophysical signal processing maximum likelihood estimation oceanographic techniques principal component analysis remote sensing by radar sea ice water synthetic aperture radar terrain mapping Electrical and Computer Engineering text 2005 ftbrighamyoung 2023-07-03T22:20:23Z A sea ice mapping algorithm for SeaWinds is developed that incorporates statistical and spatial a priori information in a modified maximum a posteriori (MAP) framework. Spatial a priori data are incorporated in the loss terms of a Bayes risk formulation. Conditional distributions and priors for sea ice and ocean statistics are represented as empirical histograms that are forced to conform to a set of expected histograms via principal component filtering. Tuning parameters for the algorithm allow adjustments in the algorithm's performance. Results of the algorithm exhibit high correlation with the Remund-Long sea ice mapping algorithm for SeaWinds and the Special Sensor Microwave/Imager National Aeronautics and Space Administration Team 30% ice edge, and are verified with RADARSAT-1 ScanSAR imagery. The resulting sea ice maps exhibit high edge detail, preserve polynyas and ice bodies disjoint from the primary ice sheet, and thus are suitable for use with wind retrieval and sea ice studies. Principles employed in the algorithm may be of interest in other classification studies. Text Ice Sheet Sea ice Brigham Young University (BYU): ScholarsArchive
institution Open Polar
collection Brigham Young University (BYU): ScholarsArchive
op_collection_id ftbrighamyoung
language English
topic Bayes methods
geophysical signal processing
maximum likelihood estimation
oceanographic techniques
principal component analysis
remote sensing by radar
sea ice
water
synthetic aperture radar
terrain mapping
Electrical and Computer Engineering
spellingShingle Bayes methods
geophysical signal processing
maximum likelihood estimation
oceanographic techniques
principal component analysis
remote sensing by radar
sea ice
water
synthetic aperture radar
terrain mapping
Electrical and Computer Engineering
Long, David G.
Anderson, Hyrum S.
Sea ice mapping method for SeaWinds
topic_facet Bayes methods
geophysical signal processing
maximum likelihood estimation
oceanographic techniques
principal component analysis
remote sensing by radar
sea ice
water
synthetic aperture radar
terrain mapping
Electrical and Computer Engineering
description A sea ice mapping algorithm for SeaWinds is developed that incorporates statistical and spatial a priori information in a modified maximum a posteriori (MAP) framework. Spatial a priori data are incorporated in the loss terms of a Bayes risk formulation. Conditional distributions and priors for sea ice and ocean statistics are represented as empirical histograms that are forced to conform to a set of expected histograms via principal component filtering. Tuning parameters for the algorithm allow adjustments in the algorithm's performance. Results of the algorithm exhibit high correlation with the Remund-Long sea ice mapping algorithm for SeaWinds and the Special Sensor Microwave/Imager National Aeronautics and Space Administration Team 30% ice edge, and are verified with RADARSAT-1 ScanSAR imagery. The resulting sea ice maps exhibit high edge detail, preserve polynyas and ice bodies disjoint from the primary ice sheet, and thus are suitable for use with wind retrieval and sea ice studies. Principles employed in the algorithm may be of interest in other classification studies.
format Text
author Long, David G.
Anderson, Hyrum S.
author_facet Long, David G.
Anderson, Hyrum S.
author_sort Long, David G.
title Sea ice mapping method for SeaWinds
title_short Sea ice mapping method for SeaWinds
title_full Sea ice mapping method for SeaWinds
title_fullStr Sea ice mapping method for SeaWinds
title_full_unstemmed Sea ice mapping method for SeaWinds
title_sort sea ice mapping method for seawinds
publisher BYU ScholarsArchive
publishDate 2005
url https://scholarsarchive.byu.edu/facpub/391
https://scholarsarchive.byu.edu/context/facpub/article/1390/viewcontent/IR_CISOPTR_713.pdf
genre Ice Sheet
Sea ice
genre_facet Ice Sheet
Sea ice
op_source Faculty Publications
op_relation https://scholarsarchive.byu.edu/facpub/391
https://scholarsarchive.byu.edu/context/facpub/article/1390/viewcontent/IR_CISOPTR_713.pdf
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