Formation and evolution of thermokarst landslides in the Qinghai-Tibet Plateau, China

Thermokarst landslide (TL) activity in the Qinghai-Tibet Plateau (QTP) is intensifying due to climate warming-induced permafrost degradation. However, the mechanisms driving landslide formation and evolution remain poorly understood. This study investigates the spatial distribution, annual frequency...

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Veröffentlicht in:	The Science of the total environment 2024-12, Vol.954, p.176557, Article 176557
Hauptverfasser:	Wei, Tao, Wang, Hao, Cui, Peng, Wang, Yan, Zhang, Bo, Wei, Rui-Long, Liu, Zhen-Xing, Li, Chao-Yue
Format:	Artikel
Sprache:	eng
Schlagworte:	Active layer detachment China climate Climate warming environment historical records ice Landslide landslides microrelief permafrost Permafrost degradation rain remote sensing Retrogressive thaw slump temperature
Online-Zugang:	Volltext
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