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 …

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

Permafrost thaw can accelerate climate warming by releasing carbon from previously frozen
soil in the form of greenhouse gases. Rainfall extremes have been proposed to increase …

We used a model for permafrost hydrology informed by detailed measurements of soil ice
content to better understand the potential risk of abrupt permafrost thaw triggered by melting …

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 …

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 …

The need to understand potential climate impacts and feedbacks in Arctic regions has
prompted recent interest in modeling of permafrost dynamics in a warming climate. A new …

Abstract Changes in snow precipitation at high latitudes can significantly affect permafrost
thermal conditions and thaw depth, potentially exposing more carbon-laden soil to microbial …

In cold and arid regions, vapor movement and water flow are crucial to thermal-moisture
dynamics of the active layer and control the soil microbial activity, plant growth and …

Taliks (perennially thawed soil in a permafrost environment) are generally found beneath
water bodies or wetlands, and their development and evolution in other environments is …