Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier

ABSTRACT Despite their importance for mass-balance estimates and the progress in techniques based on optical and thermal satellite imagery, the mapping of debris-covered glacier boundaries remains a challenging task. Manual corrections hamper regular updates. In this study, we present an automatic a...

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Published in:Journal of Glaciology
Main Authors: LIPPL, STEFAN, VIJAY, SAURABH, BRAUN, MATTHIAS
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2018
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2018.70
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000709
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spelling crcambridgeupr:10.1017/jog.2018.70 2024-09-15T18:15:39+00:00 Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier LIPPL, STEFAN VIJAY, SAURABH BRAUN, MATTHIAS 2018 http://dx.doi.org/10.1017/jog.2018.70 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000709 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 64, issue 247, page 811-821 ISSN 0022-1430 1727-5652 journal-article 2018 crcambridgeupr https://doi.org/10.1017/jog.2018.70 2024-09-04T04:04:42Z ABSTRACT Despite their importance for mass-balance estimates and the progress in techniques based on optical and thermal satellite imagery, the mapping of debris-covered glacier boundaries remains a challenging task. Manual corrections hamper regular updates. In this study, we present an automatic approach to delineate glacier outlines using interferometrically derived synthetic aperture radar (InSAR) coherence, slope and morphological operations. InSAR coherence detects the temporally decorrelated surface (e.g. glacial extent) irrespective of its surface type and separates it from the highly coherent surrounding areas. We tested the impact of different processing settings, for example resolution, coherence window size and topographic phase removal, on the quality of the generated outlines. We found minor influence of the topographic phase, but a combination of strong multi-looking during interferogram generation and additional averaging during coherence estimation strongly deteriorated the coherence at the glacier edges. We analysed the performance of X-, C- and L- band radar data. The C-band Sentinel-1 data outlined the glacier boundary with the least misclassifications and a type II error of 0.47 % compared with Global Land Ice Measurements from Space inventory data. Our study shows the potential of the Sentinel-1 mission together with our automatic processing chain to provide regular updates for land-terminating glaciers on a large scale. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 64 247 811 821
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description ABSTRACT Despite their importance for mass-balance estimates and the progress in techniques based on optical and thermal satellite imagery, the mapping of debris-covered glacier boundaries remains a challenging task. Manual corrections hamper regular updates. In this study, we present an automatic approach to delineate glacier outlines using interferometrically derived synthetic aperture radar (InSAR) coherence, slope and morphological operations. InSAR coherence detects the temporally decorrelated surface (e.g. glacial extent) irrespective of its surface type and separates it from the highly coherent surrounding areas. We tested the impact of different processing settings, for example resolution, coherence window size and topographic phase removal, on the quality of the generated outlines. We found minor influence of the topographic phase, but a combination of strong multi-looking during interferogram generation and additional averaging during coherence estimation strongly deteriorated the coherence at the glacier edges. We analysed the performance of X-, C- and L- band radar data. The C-band Sentinel-1 data outlined the glacier boundary with the least misclassifications and a type II error of 0.47 % compared with Global Land Ice Measurements from Space inventory data. Our study shows the potential of the Sentinel-1 mission together with our automatic processing chain to provide regular updates for land-terminating glaciers on a large scale.
format Article in Journal/Newspaper
author LIPPL, STEFAN
VIJAY, SAURABH
BRAUN, MATTHIAS
spellingShingle LIPPL, STEFAN
VIJAY, SAURABH
BRAUN, MATTHIAS
Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
author_facet LIPPL, STEFAN
VIJAY, SAURABH
BRAUN, MATTHIAS
author_sort LIPPL, STEFAN
title Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
title_short Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
title_full Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
title_fullStr Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
title_full_unstemmed Automatic delineation of debris-covered glaciers using InSAR coherence derived from X-, C- and L-band radar data: a case study of Yazgyl Glacier
title_sort automatic delineation of debris-covered glaciers using insar coherence derived from x-, c- and l-band radar data: a case study of yazgyl glacier
publisher Cambridge University Press (CUP)
publishDate 2018
url http://dx.doi.org/10.1017/jog.2018.70
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000709
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 64, issue 247, page 811-821
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2018.70
container_title Journal of Glaciology
container_volume 64
container_issue 247
container_start_page 811
op_container_end_page 821
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