Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway
Knowledge of the spatio-temporal occurrence of avalanche activity is critical for avalanche forecasting. We present a near-real time automatic avalanche monitoring system that outputs detected avalanche polygons within roughly 10 min after Sentinel-1 SAR data are download. Our avalanche detection al...
Published in: | Remote Sensing |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2019
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs11232863 |
_version_ | 1821662311887142912 |
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author | Markus Eckerstorfer Hannah Vickers Eirik Malnes Jakob Grahn |
author_facet | Markus Eckerstorfer Hannah Vickers Eirik Malnes Jakob Grahn |
author_sort | Markus Eckerstorfer |
collection | MDPI Open Access Publishing |
container_issue | 23 |
container_start_page | 2863 |
container_title | Remote Sensing |
container_volume | 11 |
description | Knowledge of the spatio-temporal occurrence of avalanche activity is critical for avalanche forecasting. We present a near-real time automatic avalanche monitoring system that outputs detected avalanche polygons within roughly 10 min after Sentinel-1 SAR data are download. Our avalanche detection algorithm has an average probability of detection (POD) of 67.2% with a false alarm rate (FAR) averaging 45.9, with a maximum POD of over 85% and a minimum FAR of 24.9% compared to manual detection of avalanches. The high variability in performance stems from the dynamic nature of snow in the Sentinel-1 data. After tuning parameters of the detection algorithm, we processed five years of Sentinel-1 images acquired over a 150 × 100 km large area in Northern Norway, with the best setup. Compared to a dataset of field-observed avalanches, 77.3% were manually detectable. Using these manual detections as benchmark, the avalanche detection algorithm achieved an accuracy of 79% with high POD in cases of medium to large wet snow avalanches. For the first time, we present a dataset of spatio-temporal avalanche activity over several winters from a large region. Currently, the Norwegian Avalanche Warning Service is using our processing system for pre-operational use in three regions in Norway. |
format | Text |
genre | Northern Norway |
genre_facet | Northern Norway |
geographic | Norway The Sentinel |
geographic_facet | Norway The Sentinel |
id | ftmdpi:oai:mdpi.com:/2072-4292/11/23/2863/ |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(73.317,73.317,-52.983,-52.983) |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/rs11232863 |
op_relation | https://dx.doi.org/10.3390/rs11232863 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Remote Sensing; Volume 11; Issue 23; Pages: 2863 |
publishDate | 2019 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2072-4292/11/23/2863/ 2025-01-16T23:53:50+00:00 Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway Markus Eckerstorfer Hannah Vickers Eirik Malnes Jakob Grahn agris 2019-12-02 application/pdf https://doi.org/10.3390/rs11232863 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs11232863 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 11; Issue 23; Pages: 2863 SAR Sentinel-1 snow avalanche automatic detection Text 2019 ftmdpi https://doi.org/10.3390/rs11232863 2023-07-31T22:51:11Z Knowledge of the spatio-temporal occurrence of avalanche activity is critical for avalanche forecasting. We present a near-real time automatic avalanche monitoring system that outputs detected avalanche polygons within roughly 10 min after Sentinel-1 SAR data are download. Our avalanche detection algorithm has an average probability of detection (POD) of 67.2% with a false alarm rate (FAR) averaging 45.9, with a maximum POD of over 85% and a minimum FAR of 24.9% compared to manual detection of avalanches. The high variability in performance stems from the dynamic nature of snow in the Sentinel-1 data. After tuning parameters of the detection algorithm, we processed five years of Sentinel-1 images acquired over a 150 × 100 km large area in Northern Norway, with the best setup. Compared to a dataset of field-observed avalanches, 77.3% were manually detectable. Using these manual detections as benchmark, the avalanche detection algorithm achieved an accuracy of 79% with high POD in cases of medium to large wet snow avalanches. For the first time, we present a dataset of spatio-temporal avalanche activity over several winters from a large region. Currently, the Norwegian Avalanche Warning Service is using our processing system for pre-operational use in three regions in Norway. Text Northern Norway MDPI Open Access Publishing Norway The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) Remote Sensing 11 23 2863 |
spellingShingle | SAR Sentinel-1 snow avalanche automatic detection Markus Eckerstorfer Hannah Vickers Eirik Malnes Jakob Grahn Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title | Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title_full | Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title_fullStr | Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title_full_unstemmed | Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title_short | Near-Real Time Automatic Snow Avalanche Activity Monitoring System Using Sentinel-1 SAR Data in Norway |
title_sort | near-real time automatic snow avalanche activity monitoring system using sentinel-1 sar data in norway |
topic | SAR Sentinel-1 snow avalanche automatic detection |
topic_facet | SAR Sentinel-1 snow avalanche automatic detection |
url | https://doi.org/10.3390/rs11232863 |