Arctic‐boreal landscapes are experiencing profound warming, along with changes in
ecosystem moisture status and disturbance from fire. This region is of global importance in …

Abstract Small water bodies (< 0.01 km 2) showing diverse limnological properties occur in
great abundance across the boreal forest and tundra landscapes of the Arctic and Subarctic …

The continued warming of the Arctic could release vast stores of carbon into the atmosphere
from high-latitude ecosystems, especially from thawing permafrost. Increasing uptake of …

Arctic warming causes permafrost thaw and accelerates microbial decomposition of soil
organic matter (SOM) to carbon dioxide (CO2) and methane (CH4). The determining factors …

Climate change poses a serious threat to permafrost integrity, with expected warmer winters
and increased precipitation, both raising permafrost temperatures and active layer thickness …

Contrary to the general “greening of the Arctic”, the Siberian Indigirka Lowlands show strong
“browning”(a decrease in the Normalized Difference Vegetation Index or “NDVI”) in various …

We employ a new, process-based model for methane emissions from ponds (MeEP) to
investigate the methane-emission response of polygonal-tundra ponds in Northeast Siberia …

Permafrost-affected soils contain large quantities of soil organic carbon (SOC). Changes in
the SOC pool of a particular ecosystem can be related to its net ecosystem carbon balance …

Despite the importance of small and medium size rivers of Siberian boreal zone in
greenhouse gases (GHG) emission, major knowledge gaps exist regarding its temporal …

Landscapes are often assumed to be homogeneous when interpreting eddy covariance
fluxes, which can lead to biases when gap-filling and scaling up observations to determine …