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

Arctic coasts are vulnerable to the effects of climate change, including rising sea levels and
the loss of permafrost, sea ice and glaciers. Assessing the influence of anthropogenic …

Permafrost is a sub-ground phenomenon and therefore cannot be directly observed from
space. It is an Essential Climate Variable and associated with climate tipping points. Multi …

Observational data of coastal change over much of the Arctic are limited largely due to its
immensity, remoteness, harsh environment, and restricted periods of sunlight and ice-free …

Increasing Arctic temperatures accelerate coastal erosion, threatening coastal communities
and infrastructure, and adding carbon to the atmosphere. Research now predicts that Arctic …

The Arctic is experiencing rapid warming, which among other processes results in
increasing erosion of coastal permafrost and the release of ancient organic carbon (OC) into …

Arctic river deltas and deltaic near-shore zones represent important land–ocean transition
zones influencing sediment dynamics and nutrient fluxes from permafrost-affected terrestrial …

Unoccupied aerial systems (UAS) are an established technique for collecting data on cold
region phenomenon at high spatial and temporal resolutions. While many studies have …

This report presents an overview of the costal erosion model and the infrastructure stability
model that are capable of predicting the site-specific response to the global warming and …

Arctic shorelines are vulnerable to climate change impacts as sea level rises, permafrost
thaws, storms intensify, and sea ice thins. Seventy-five years of aerial and satellite …