Yedoma is a permafrost deposit widely distributed across the Arctic and found exclusively
within the unglaciated regions in northern Siberia, Alaska, and the Yukon, which are the …

Permafrost-affected tundra soils are large carbon (C) and nitrogen (N) reservoirs. However,
N is largely bound in soil organic matter (SOM), and ecosystems generally have low N …

Significant attention has been given to the way in which the soil nitrogen (N) cycle responds
to permafrost thaw in recent years, yet little is known about anaerobic N transformations in …

Tundra and boreal ecosystems encompass the northern circumpolar permafrost region and
are experiencing rapid environmental change with important implications for the global …

Wetlands in Arctic drained lake basins (DLBs) have a high potential for carbon storage in
vegetation and peat as well as for elevated greenhouse gas emissions. However, the …

Snow is critically important to the energy budget, biogeochemistry, ecology, and people of
the Arctic. While climate change continues to shorten the duration of the snow cover period …

Accelerating permafrost thaw across high-latitude ecosystems increases organic matter
(OM) availability to soil microorganisms. The chemical composition of permafrost-derived …

Climate change in the Arctic is altering watershed hydrologic processes and
biogeochemistry. Here, we present an emergent threat to Arctic watersheds based on …

The Arctic is experiencing dramatic climate‐induced changes, which could have substantial
consequences for nutrient export from land to streams and, thus, in‐stream nutrient …

Abstract The Arctic Ocean and adjacent seas are undergoing increased freshwater influx
due to enhanced glacial and sea ice melt, precipitation, and runoff. Accurate delineation of …