The first hillslope thermokarst inventory for the permafrost region of the Qilian Mountains

• Published in: Earth system science data Vol. 16; no. 4; pp. 2033 - 2045
• Main Authors: Peng, Xiaoqing, Yang, Guangshang, Frauenfeld, Oliver W, Li, Xuanjia, Tian, Weiwei, Chen, Guanqun, Huang, Yuan, Wei, Gang, Luo, Jing, Mu, Cuicui, Niu, Fujun
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 29-04-2024; Copernicus Publications
• Subjects: Anthropogenic factors; Climate change; Cold regions; Datasets; Degradation; Earthquakes; Economic impact; Ecosystem disturbance; Geomorphology; Global warming; Gullies; Gully erosion; Mountains; Permafrost; Precipitation; Regions; Remote sensing; River basins; Seismic engineering; Slump structures; Software; Soil degradation; Solar radiation; Thermokarst; Thickness; Vegetation; Visual fields; Canada; Tibetan Plateau; Arctic region
• ISSN: 1866-3516; 1866-3508; 1866-3516
• DOI: 10.5194/essd-16-2033-2024

Climate warming and anthropogenic disturbances result in permafrost degradation in cold regions, including in the Qilian Mountains. These changes lead to extensive hillslope thermokarst (HT) formation, such as retrogressive thaw slumps, active-layer detachment slides, and thermal erosion gullies. These in turn cause, e.g., degradation of local vegetation, economic losses, infrastructure damages, and threats to human safety. However, despite its importance, there is currently no thermokarst inventory for the Qilian Mountains. Through manual visual interpretation and field validation, we therefore produce the first quantification of HT features. We count a total of 1064 HT features, with 67 % located in the upper reaches of the Heihe River basin, which encompasses ∼ 13 % of the Qilian Mountains region. We further identified that 187 HT features (18 %) existed before 2010, while the remaining 874 (82 %) were initiated in the recent period. More specifically, 392 sites (37 %) were initiated during 2010–2015 and 482 (45 %) after 2015. Thermokarst terrain is observed primarily in areas with shallow active-layer depths (average thickness 2.98 m) on northern shaded slopes of 3–25°, with low solar radiation and moderate elevations ranging from 3200 to 4000 m. This first inventory of HT features is an important and missing piece in documenting changes on the Qinghai–Tibetan Plateau, and this new dataset also provides an important basis for further studies, such as automated extraction of HT features, susceptibility analysis of HT, and estimation of losses caused by HT. The datasets are available from the National Tibetan Plateau/Third Pole Environment Data Center and can be downloaded from https://doi.org/10.11888/Cryos.tpdc.300805 (Peng and Yang, 2023).