Landslides induced by freeze–thaw processes on grasslands are one of the major
geohazards, and their scale and frequency are increasing as the global warms. Freeze-thaw …

With the expansion of engineering activities, numerous major projects are gradually
emerging in frozen soil regions. However, due to the unique engineering properties of …

Identifying the changes in thermokarst lake dynamics has a significant contribution to
landscape‐scale hydrology, ecology, and assessment of carbon budgets in permafrost …

Warm permafrost sites such as those extensively existing on the Qinghai-Tibet Plateau
present a challenging geological environment for infrastructure engineering. A reliable …

Surface water is an important local factor in engineering geological conditions in permafrost
regions. In this paper, the impacts of surface water ponding on the long-term thermal and …

The lakes distributed in permafrost areas on the Tibetan Plateau (TP) have been
experiencing significant changes during the past few decades as a result of the climate …

In permafrost regions of the Qinghai-Tibet Plateau, road disaster caused by permafrost
degradation cannot be ignored. As a common thermal disaster in permafrost regions …

In cold regions, the thermal effect of accumulated water on underlying permafrost and
permafrost subgrade remains a significant hazard causing engineering risks. Water depth of …

Hydro-thermal coupling is the essence of the freeze-thaw process, and theoretical studies of
this coupled process have been hot topics in the field of frozen soil. Darcy's law of …

Buried pipelines are widely used for transporting oil in remote cold regions. However, the
warm oil can induce considerable thermal influence on the surrounding frozen soils and …