Permafrost thaw can cause an intensification of climate change through the release of
carbon as greenhouse gases. While the effect of air temperature on permafrost thaw is well …

The impacts of ongoing climate warming on cold‐regions hydrogeology and groundwater
resources have created a need to develop groundwater models adapted to these …

Nordenskiöld Land in Central Spitsbergen, Svalbard is characterized as a high latitude, high
relief periglacial landscape with permafrost occurring both in mountains and lowlands …

Active layer probing in northern Sweden, northeast Greenland, and central Svalbard
indicates active layer thickening has occurred at Circumpolar Active Layer Monitoring …

Through taliks—thawed zones extending through the entire permafrost layer—represent a
critical type of heterogeneity that affects water redistribution and heat transport, especially in …

Thicker snow cover in permafrost areas causes deeper active layers and thaw subsidence,
which alter local hydrology and may amplify the loss of soil carbon. However, the potential …

Abstract Study Region Yangpota Mountain in Zhuanglang County, Loess Plateau Hilly Area.
Study Focus In dry and degraded ecosystems, water scarcity remains the most significant …

The CryoGrid community model is a flexible toolbox for simulating the ground thermal
regime and the ice–water balance for permafrost and glaciers, extending a well-established …

The hydrothermal changes in the active layers of permafrost soils during freeze–thaw
processes are crucial for understanding the interactions between the surface and the …

Modeling the physical state of permafrost landscapes is a crucial addition to field
observations in order to understand the feedback mechanisms between permafrost and the …