Abstract The Tibetan Plateau (TP) has the largest permafrost area in the low-and mid-
latitudes. With warmer ground temperatures and ice-rich terrain, the TP permafrost is …

Cryospheric hazards-in this case, thaw slumps (TS) and thermo-erosion gullies (TEG)-are
phenomena typical of permafrost-dominated landscapes. Open datasets informing about …

Deep‐learning (DL) models have become increasingly beneficial for the detection of
retrogressive thaw slumps (RTS) in the permafrost domain. However, comparing accuracy …

Landslides, which can occur due to earthquakes and heavy rainfall, pose significant
challenges across large areas. To effectively manage these disasters, it is crucial to have …

Retrogressive thaw slumps (RTS) are a form of abrupt permafrost thaw that can rapidly
mobilize ancient frozen soil carbon, magnifying the permafrost carbon feedback. However …

Arctic permafrost is undergoing rapid changes due to climate warming in high latitudes.
Retrogressive thaw slumps (RTS) are one of the most abrupt and impactful thermal …

Arctic permafrost is facing significant changes due to global climate change. As these
regions are largely inaccessible, remote sensing plays a crucial rule in better understanding …

Retrogressive thaw slumps (RTSs), formed by abrupt degradation of ice‐rich permafrost, are
widely distributed on the Qinghai‐Tibet Plateau, causing infrastructure damage and …

Climate warming and anthropogenic disturbances result in permafrost degradation in cold
regions, including in the Qilian Mountains. These changes lead to extensive hillslope …

This chapter investigates the significant role of artificial intelligence (AI)-supported remote
sensing (RS) studies in the polar cryosphere, focusing on both Antarctica and the Arctic …