Retrogressive thaw slumps (RTSs) have become a dominant geomorphic event in
permafrost regions due to the modern climate change. However, the roles of topographic …

Climate change affects cryosphere-fed rivers and alters seasonal sediment dynamics,
affecting cyclical fluvial material supply and year-round water-food-energy provisions to …

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

Fine-grained muds produced largely from rock weathering at the Earth's surface have great
influence on global carbon cycling. Mud binds and protects organic carbon (OC) from …

Global glacier mass loss has accelerated, producing more and larger glacial lakes. Many of
these glacial lakes are a source of glacial lake outburst floods (GLOFs), which pose threats …

Stream networks in Arctic and high-elevation regions underlain by frozen ground (ie,
permafrost) are expanding and developing in response to accelerating global warming, and …

Recent climate change has caused an increase in warming-driven erosion and sediment
transport processes on the Tibetan Plateau (TP). Yet a lack of measurements hinders our …

Glacial lakes can form and grow due to glacial retreat, and rapid lake drainage can produce
destructive floods. Outburst flood compilations show a temporal increase in frequency; …

Most cryospheric ecosystems are energy limited. How their energetics will respond to
climate change remains largely unknown. This is particularly true for glacier-fed streams …

Abstract The early Eocene (~ 56–48 million years ago) was marked by peak Cenozoic
warmth and sea levels, high CO2, and largely ice-free conditions. This time has been …