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 Arctic region is the most sensitive region to climate change. Hydrological models are
fundamental tools for climate change impact assessment. However, due to the extreme …

Frozen depth has a great significance for the foundation engineering in cold regions, always
showing a high correlation with some attendant engineering phenomena, including water …

Cold regions involve hydrological processes that are not often addressed appropriately in
hydrological models. The Cold Regions Hydrological Modelling platform (CRHM) was …

Fire is an important factor controlling the composition and thickness of the organic layer in
the black spruce forest ecosystems of interior Alaska. Fire that burns the organic layer can …

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 …

Simulations of maximum annual thaw at a continuous and a discontinuous permafrost site in
Canada were performed using Community Land Model version 3 (CLM3) and randomized …

Ground thawing and freezing depths (GTFDs) strongly influence the hydrology and energy
balances of permafrost regions. Current methods to simulate GTFD differ in algorithm type …

Thermokarst lakes alter landscape topography and hydrology in widespread permafrost
regions and mobilize significant permafrost carbon pools, including releasing methane …

Snow and frozen soil prevail in cold regions worldwide, and the integration of these
processes is crucial in hydrological models. In this study, a combined model was developed …