A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea

In this study, we pursue two objectives: first, we compare six different “constant false alarm rate” (CFAR) algorithms for iceberg detection in SAR images, and second, we investigate the effect of radar frequency by comparing the detection performance at C- and L-band. The SAR images were acquired o...

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Published in:The Cryosphere
Main Authors: Færch, Laust, Dierking, Wolfgang, Hughes, Nick, Doulgeris, Anthony P.
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-5335-2023
https://tc.copernicus.org/articles/17/5335/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc109353 2024-01-14T10:08:29+01:00 A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea Færch, Laust Dierking, Wolfgang Hughes, Nick Doulgeris, Anthony P. 2023-12-15 application/pdf https://doi.org/10.5194/tc-17-5335-2023 https://tc.copernicus.org/articles/17/5335/2023/ eng eng doi:10.5194/tc-17-5335-2023 https://tc.copernicus.org/articles/17/5335/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-5335-2023 2023-12-18T17:24:16Z In this study, we pursue two objectives: first, we compare six different “constant false alarm rate” (CFAR) algorithms for iceberg detection in SAR images, and second, we investigate the effect of radar frequency by comparing the detection performance at C- and L-band. The SAR images were acquired over the Labrador Sea under melting conditions. In an overlapping optical Sentinel-2 image, 492 icebergs were identified in the area. They were used for an assessment of the algorithms' capabilities to accurately detect them in the SAR images and for the determination of the number of false alarms and missed detections. By testing the detectors at varying probability of false alarm (PFA) levels, the optimum PFA for each detector was found. Additionally, we considered the effect of iceberg sizes in relation to image resolution. The results showed that the overall highest accuracy was achieved by applying a log-normal CFAR detector to the L-band image ( F score of 70.4 %), however, only for a narrow range of PFA values. Three of the tested detectors provided high F scores above 60 % over a wider range of PFA values both at L- and C-band. Low F scores were mainly caused by missed detections of small-sized ( < 60 m) and medium-sized (60–120 m) icebergs, with approximately 20 %–40 % of the medium icebergs and 85 %–90 % of small icebergs being missed by all detectors. The iDPolRAD detector, which is sensitive to volume scattering, is less suitable under melting conditions. Text Labrador Sea Copernicus Publications: E-Journals The Cryosphere 17 12 5335 5355
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In this study, we pursue two objectives: first, we compare six different “constant false alarm rate” (CFAR) algorithms for iceberg detection in SAR images, and second, we investigate the effect of radar frequency by comparing the detection performance at C- and L-band. The SAR images were acquired over the Labrador Sea under melting conditions. In an overlapping optical Sentinel-2 image, 492 icebergs were identified in the area. They were used for an assessment of the algorithms' capabilities to accurately detect them in the SAR images and for the determination of the number of false alarms and missed detections. By testing the detectors at varying probability of false alarm (PFA) levels, the optimum PFA for each detector was found. Additionally, we considered the effect of iceberg sizes in relation to image resolution. The results showed that the overall highest accuracy was achieved by applying a log-normal CFAR detector to the L-band image ( F score of 70.4 %), however, only for a narrow range of PFA values. Three of the tested detectors provided high F scores above 60 % over a wider range of PFA values both at L- and C-band. Low F scores were mainly caused by missed detections of small-sized ( < 60 m) and medium-sized (60–120 m) icebergs, with approximately 20 %–40 % of the medium icebergs and 85 %–90 % of small icebergs being missed by all detectors. The iDPolRAD detector, which is sensitive to volume scattering, is less suitable under melting conditions.
format Text
author Færch, Laust
Dierking, Wolfgang
Hughes, Nick
Doulgeris, Anthony P.
spellingShingle Færch, Laust
Dierking, Wolfgang
Hughes, Nick
Doulgeris, Anthony P.
A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
author_facet Færch, Laust
Dierking, Wolfgang
Hughes, Nick
Doulgeris, Anthony P.
author_sort Færch, Laust
title A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
title_short A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
title_full A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
title_fullStr A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
title_full_unstemmed A comparison of constant false alarm rate object detection algorithms for iceberg identification in L- and C-band SAR imagery of the Labrador Sea
title_sort comparison of constant false alarm rate object detection algorithms for iceberg identification in l- and c-band sar imagery of the labrador sea
publishDate 2023
url https://doi.org/10.5194/tc-17-5335-2023
https://tc.copernicus.org/articles/17/5335/2023/
genre Labrador Sea
genre_facet Labrador Sea
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-5335-2023
https://tc.copernicus.org/articles/17/5335/2023/
op_doi https://doi.org/10.5194/tc-17-5335-2023
container_title The Cryosphere
container_volume 17
container_issue 12
container_start_page 5335
op_container_end_page 5355
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