TY - JOUR
T1 - A Labeling Intercomparison of Retrogressive Thaw Slumps by a Diverse Group of Domain Experts
AU - Nitze, Ingmar
AU - Van der Sluijs, Jurjen
AU - Barth, Sophia
AU - Bernhard, Philipp
AU - Huang, Lingcao
AU - Kizyakov, Alexander
AU - Lara, Mark J
AU - Nesterova, Nina
AU - Runge, Alexandra
AU - Veremeeva, Alexandra
AU - Ward Jones, Melissa
AU - Witharana, Chandi
AU - Xia, Zhuoxuan
AU - Liljedahl, Anna K
N1 - We thank the International Permafrost Association for funding to support in-person meetings and for recognizing this community driven initiative through the IPA Action Group RTSInTrain. PlanetScope commercial satellite data were acquired through the HGF AI-CORE Project. Action group funding by IPA IN funded by NSF (awards #1927872 and #2052107), HGF AI-CORE (also Planet commercial data), ESA CCI + Permafrost, and BMWK ML4EARTH. AK was funded by the MSU research program \u201CThe cryosphere evolution under climate change and anthropogenic impact\u201D (#121051100164-0). NN was funded by a DAAD fellowship (Grant #57588368). MJL was supported by NSF-EnvE (1927772) and NASA-ABoVE (80NSSC22K1254). AL funded by NSF awards to develop the Permafrost Discovery Gateway (awards #1927872 #2052107). CW funded by NSF awards to develop the Permafrost Discovery Gateway (award #1927723). AR was funded by the ESA CCI postdoctoral fellowship (ESA Contract No. 4000134121/21/I-NB).
This study was funded by the International Permafrost Association (RTSInTrainActionGroup). Individual contributors were supported by Helmholtz Association (AI\u2010CORE), German Federal Ministry for Economic Affairs and Climate Action (ML4Earth50EE2201C), National Science Foundation (1927723, 1927772, 1927872 and 2052107), European Space Agency (CCI+Permafrost, ESA CCI postdoctoral fellowship 4000134121/21/I\u2010NB), Lomonosov Moscow State University (121051100164\u20100), German Academic Exchange Service (57588368), and National Aeronautics and Space Administration (80NSSC22K1254). Funding:
We thank the International Permafrost Association for funding to support in\u2010person meetings and for recognizing this community driven initiative through the IPA Action Group . PlanetScope commercial satellite data were acquired through the HGF AI\u2010CORE Project. Action group funding by IPA IN funded by NSF (awards #1927872 and #2052107), HGF AI\u2010CORE (also Planet commercial data), ESA CCI\u2009+\u2009Permafrost, and BMWK ML4EARTH. AK was funded by the MSU research program \u201CThe cryosphere evolution under climate change and anthropogenic impact\u201D (#121051100164\u20100). NN was funded by a DAAD fellowship (Grant #57588368). MJL was supported by NSF\u2010EnvE (1927772) and NASA\u2010ABoVE (80NSSC22K1254). AL funded by NSF awards to develop the Permafrost Discovery Gateway (awards #1927872 #2052107). CW funded by NSF awards to develop the Permafrost Discovery Gateway (award #1927723). AR was funded by the ESA CCI postdoctoral fellowship (ESA Contract No. 4000134121/21/I\u2010NB). RTSInTrain
PY - 2025
Y1 - 2025
N2 - Deep-learning (DL) models have become increasingly beneficial for the detection of retrogressive thaw slumps (RTS) in the permafrost domain. However, comparing accuracy metrics is challenging due to unstandardized labeling guidelines. To address this, we conducted an experiment with 12 international domain experts from a broad range of scientific backgrounds. Using 3 m PlanetScope multispectral imagery, they digitized RTS footprints in two sites. We evaluated label uncertainty by comparing manually outlined RTS labels using Intersection-over-Union (IoU) and F1 metrics. At the Canadian Peel Plateau site, we see good agreement, particularly in the active parts of RTS. Differences were observed in the interpretation of the debris tongue and the stable vegetated sections of RTS. At the Russian Bykovsky site, we observed a larger mismatch. Here, the same differences were documented, but several participants mistakenly identified non-RTS features. This emphasizes the importance of site-specific knowledge for reliable label creation. The experiment highlights the need for standardized labeling procedures and definition of their scientific purpose. The most similar expert labels outperformed the accuracy metrics reported in the literature, highlighting human labeling capabilities with proper training, site knowledge, and clear guidelines. These findings lay the groundwork for DL-based RTS monitoring in the pan-Arctic.
AB - Deep-learning (DL) models have become increasingly beneficial for the detection of retrogressive thaw slumps (RTS) in the permafrost domain. However, comparing accuracy metrics is challenging due to unstandardized labeling guidelines. To address this, we conducted an experiment with 12 international domain experts from a broad range of scientific backgrounds. Using 3 m PlanetScope multispectral imagery, they digitized RTS footprints in two sites. We evaluated label uncertainty by comparing manually outlined RTS labels using Intersection-over-Union (IoU) and F1 metrics. At the Canadian Peel Plateau site, we see good agreement, particularly in the active parts of RTS. Differences were observed in the interpretation of the debris tongue and the stable vegetated sections of RTS. At the Russian Bykovsky site, we observed a larger mismatch. Here, the same differences were documented, but several participants mistakenly identified non-RTS features. This emphasizes the importance of site-specific knowledge for reliable label creation. The experiment highlights the need for standardized labeling procedures and definition of their scientific purpose. The most similar expert labels outperformed the accuracy metrics reported in the literature, highlighting human labeling capabilities with proper training, site knowledge, and clear guidelines. These findings lay the groundwork for DL-based RTS monitoring in the pan-Arctic.
KW - deep learning
KW - hillslope thermokarst
KW - permafrost
KW - remote sensing
KW - retrogressive thaw slumps
KW - uncertainty estimation
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U2 - 10.1002/ppp.2249
DO - 10.1002/ppp.2249
M3 - Article
AN - SCOPUS:85206880319
SN - 1045-6740
VL - 36
SP - 83
EP - 92
JO - Permafrost and Periglacial Processes
JF - Permafrost and Periglacial Processes
IS - 1
ER -