Permafrost is warming globally which leads to widespread permafrost thaw. Particularly ice- rich permafrost is vulnerable to rapid thaw and erosion, impacting whole landscapes and …
Cryospheric hazards-in this case, thaw slumps (TS) and thermo-erosion gullies (TEG)-are phenomena typical of permafrost-dominated landscapes. Open datasets informing about …
In response to increasing Arctic temperatures, ice-rich permafrost landscapes are undergoing rapid changes. In permafrost lowlands, polygonal ice wedges are especially …
RD Șerban, M Șerban, R He, H Jin, Y Li, X Li, X Wang… - Remote Sensing, 2021 - mdpi.com
Land use and cover changes (LUCC) in permafrost regions have significant consequences on ecology, engineered systems, and the environment. Obtaining more details about LUCC …
A Pastukhov, T Marchenko-Vagapova, S Loiko… - Plants, 2021 - mdpi.com
Based on the data of the plant macrofossil and palynological composition of the peat deposits, the evolution and current state of polygonal peatlands were analyzed at the …
FJ Cuesta-Valero, H Beltrami… - Earth System …, 2022 - esd.copernicus.org
Heat storage within the Earth system is a fundamental metric for understanding climate change. The current energy imbalance at the top of the atmosphere causes changes in …
Rapid global warming is catalyzing widespread permafrost degradation in the Arctic, leading to destructive land-surface subsidence that destabilizes and deforms the ground …
Erosion-induced lateral soil redistribution leads to spatially heterogenous soil composition, which can be captured through the distinctive spectral reflectance of soils under varying …
Soil-geomorphological mapping is a reliable tool for analyzing the patterns of soil distribution in various parts of Earth's surface. Cryogenic and watershed areas are the most …