Rapid atmospheric warming since the mid-twentieth century has increased temperature-
dependent erosion and sediment-transport processes in cold environments, affecting food …

Bank retreat plays a fundamental role in fluvial and estuarine dynamics. It affects the cross‐
sectional evolution of channels, provides a source of sediment, and modulates the diversity …

Arctic regions are disproportionately affected by atmospheric warming, with cascading
effects on multiple surface processes. Atmospheric warming is destabilizing permafrost …

This paper discusses the potential response of fluvial processes and landforms to the
projected permafrost degradation and related hydrological change. Fluvial system structure …

The Lena, a large river that drains the northern coldest region of the Northern Hemisphere,
is deeply influenced by the continuous permafrost and degradation of the frozen ground has …

River meandering and lateral migration, caused by riverbank erosion, is a major global
threat to soil, sediment, lands, and habitats. However, compared to the densely populated …

During the breakup of river ice covers, a greater potential for erosion occurs due to rising
discharge and moving ice and the highly dynamic waves that form upon ice-jam release …

This article presents a review of previous studies on the impacts of climate change and the
operation of dam reservoirs on the characteristics of river ice cover. Based on a review of the …

Whether permafrost systematically alters the rate of riverbank erosion is a fundamental
geomorphic question with significant importance to infrastructure, water quality, and …

Over the past decades, riparian land-use changes coupled to the multiplication of river
infrastructures have enhanced vulnerability issues for societies and ecosystems located …