Where present, permafrost exerts a primary control on water fluxes, flowpaths, and
distribution. Climate warming and related drivers of soil thermal change are expected to …

Under a warming climate, permafrost degradation has resulted in profound hydrogeological
consequences. Here, we mainly review 240 recent relevant papers. Permafrost degradation …

This study investigates and compares soil moisture and hydrology projections of broadly
used land models with permafrost processes and highlights the causes and impacts of …

Permafrost is a distinct feature of the terrestrial Arctic and is vulnerable to climate warming.
Permafrost degrades in different ways, including deepening of a seasonally unfrozen …

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 …

Peatlands are wetlands that provide important ecosystem services including carbon
sequestration and water storage that respond to hydrological, biological, and …

Permafrost thaw due to climate warming modifies hydrological processes by increasing
hydrological connectivity between aquifers and surface water bodies and increasing …

Frozen ground has an important role in regional hydrological cycles and ecosystems,
particularly on the Qinghai–Tibetan Plateau (QTP), which is characterized by high elevations …

In high-elevation, boreal and arctic regions, hydrological processes and associated water
bodies can be strongly influenced by the distribution of permafrost. Recent field and …

Seasonally frozen ground (SFG) and permafrost underlay approximately half of the land
surface in the Northern Hemisphere. It is anticipated that climate warming will degrade both …