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

Arctic Science

article

Lindsay Armstrong¹  Denis Lacelle¹  Robert H. Fraser²  Steve Kokelj³  Anders Knudby¹ 

[1] Department of Geography, University of Ottawa;Canada Centre for Mapping and Earth Observation;Northwest Territories Geological Survey, Government of Northwest Territories

关键词: thermokarst;    permafrost;    remote sensing;    Arctic.;   

DOI  :  10.1139/as-2018-0016

学科分类：地球科学(综合)

来源: NRC Research Press

【 摘 要 】

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.

【 授权许可】

CC BY