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

Climate change is expected to reduce water security in arid mountain regions around the
world. Vulnerable water supplies in semi-arid zones, such as the Dry Andes, are projected to …

Lateral CH4 inputs to Arctic lakes through groundwater discharge could be substantial and
constitute an important pathway that links CH4 production in thawing permafrost to …

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

As permafrost thaws in the Arctic, new subsurface pathways open for the transport of
groundwater, energy, and solutes. We identify different ways that these subsurface changes …

Abstract A two-dimensional (2D) cryo-hydrogeological numerical model of groundwater flow,
coupled with advective-conductive heat transport with phase change, has been developed …

In continuous permafrost environments, understanding complex river‐talik system dynamics
is fundamental for the sustainable use of talik aquifers as a source of drinking water in …

Among the few positive impacts of climate warming in cold regions, permafrost degradation
can increase the availability of groundwater as a potential source of drinking water for …

Groundwater-surface water (GW-SW) interaction, as a key component in the cold region
hydrologic cycle, is extremely sensitive to seasonal and climate change. Specifically, the …

Hydrogeochemical data are used to better understand recharge dynamics and to support a
hydrogeological conceptual model in a 2-km 2 watershed in a discontinuous permafrost …