Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry

Thaw slumps are one of the most dynamic features in permafrost terrain. Improved temporal and spatial resolution monitoring of slump activity is required to better characterize their dynamics over the thaw season. We assess how a ground-based stationary camera array in a time-lapse configuration can...

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Published in:Arctic Science
Main Authors: Armstrong, Lindsay, Lacelle, Denis, Fraser, Robert H., Kokelj, Steve, Knudby, Anders
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2018
Subjects:
Online Access:http://dx.doi.org/10.1139/as-2018-0016
https://cdnsciencepub.com/doi/full-xml/10.1139/as-2018-0016
https://cdnsciencepub.com/doi/pdf/10.1139/as-2018-0016
id crcansciencepubl:10.1139/as-2018-0016
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spelling crcansciencepubl:10.1139/as-2018-0016 2024-09-15T17:49:58+00:00 Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry Armstrong, Lindsay Lacelle, Denis Fraser, Robert H. Kokelj, Steve Knudby, Anders 2018 http://dx.doi.org/10.1139/as-2018-0016 https://cdnsciencepub.com/doi/full-xml/10.1139/as-2018-0016 https://cdnsciencepub.com/doi/pdf/10.1139/as-2018-0016 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Arctic Science volume 4, issue 4, page 827-845 ISSN 2368-7460 2368-7460 journal-article 2018 crcansciencepubl https://doi.org/10.1139/as-2018-0016 2024-08-22T04:08:45Z Thaw slumps are one of the most dynamic features in permafrost terrain. Improved temporal and spatial resolution monitoring of slump activity is required to better characterize their dynamics over the thaw season. We assess how a ground-based stationary camera array in a time-lapse configuration can be integrated with unmanned aerial vehicle (UAV)-based surveys and Structure-from-Motion processing to monitor the activity of thaw slumps at high temporal and spatial resolutions. We successfully constructed point-clouds and digital surface models of the headwall area of a thaw slump at 6- to 13-day intervals over the summer, significantly improving the decadal to annual temporal resolution of previous studies. The successfully modeled headwall portion of the slump revealed that headwall retreat rates were significantly correlated with mean daily air temperature, thawing degree-days, and average net short-wave radiation and suggest a two-phased slump activity. The main challenges were related to strong JPEG image compression, drifting camera clocks, and highly dynamic nature of the feature. Combined with annual UAV-based surveys, the proposed methodology can address temporal gaps in our understanding of factors driving thaw slump activity. Such insight could help predict how slumps could modify their behavior under changing climate. Article in Journal/Newspaper Arctic permafrost Canadian Science Publishing Arctic Science 4 4 827 845
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Thaw slumps are one of the most dynamic features in permafrost terrain. Improved temporal and spatial resolution monitoring of slump activity is required to better characterize their dynamics over the thaw season. We assess how a ground-based stationary camera array in a time-lapse configuration can be integrated with unmanned aerial vehicle (UAV)-based surveys and Structure-from-Motion processing to monitor the activity of thaw slumps at high temporal and spatial resolutions. We successfully constructed point-clouds and digital surface models of the headwall area of a thaw slump at 6- to 13-day intervals over the summer, significantly improving the decadal to annual temporal resolution of previous studies. The successfully modeled headwall portion of the slump revealed that headwall retreat rates were significantly correlated with mean daily air temperature, thawing degree-days, and average net short-wave radiation and suggest a two-phased slump activity. The main challenges were related to strong JPEG image compression, drifting camera clocks, and highly dynamic nature of the feature. Combined with annual UAV-based surveys, the proposed methodology can address temporal gaps in our understanding of factors driving thaw slump activity. Such insight could help predict how slumps could modify their behavior under changing climate.
format Article in Journal/Newspaper
author Armstrong, Lindsay
Lacelle, Denis
Fraser, Robert H.
Kokelj, Steve
Knudby, Anders
spellingShingle Armstrong, Lindsay
Lacelle, Denis
Fraser, Robert H.
Kokelj, Steve
Knudby, Anders
Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
author_facet Armstrong, Lindsay
Lacelle, Denis
Fraser, Robert H.
Kokelj, Steve
Knudby, Anders
author_sort Armstrong, Lindsay
title Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
title_short Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
title_full Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
title_fullStr Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
title_full_unstemmed Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry
title_sort thaw slump activity measured using stationary cameras in time-lapse and structure-from-motion photogrammetry
publisher Canadian Science Publishing
publishDate 2018
url http://dx.doi.org/10.1139/as-2018-0016
https://cdnsciencepub.com/doi/full-xml/10.1139/as-2018-0016
https://cdnsciencepub.com/doi/pdf/10.1139/as-2018-0016
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_source Arctic Science
volume 4, issue 4, page 827-845
ISSN 2368-7460 2368-7460
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/as-2018-0016
container_title Arctic Science
container_volume 4
container_issue 4
container_start_page 827
op_container_end_page 845
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