Soil organic carbon (SOC) stored in northern peatlands and permafrost-affected soils are
key components in the global carbon cycle. This article quantifies SOC stocks in a sub-Arctic …

Soils in the northern high latitudes are a key component in the global carbon cycle; the
northern permafrost region covers 22% of the Northern Hemisphere and holds almost twice …

Ponds and lakes are abundant in Arctic permafrost lowlands. They play an important role in
Arctic wetland ecosystems by regulating carbon, water, and energy fluxes and providing …

Organic carbon (OC) stored in permafrost affected soils of the higher northern latitudes is
known to be highly vulnerable to ongoing climatic change. Although the ways to quantify soil …

To project the future development of the soil organic carbon (SOC) storage in permafrost
environments, the spatial and vertical distribution of key soil properties and their landscape …

Interactions between minerals and organic carbon (OC) in soils are key to stabilize OC and
mitigate greenhouse gas emissions upon permafrost thaw. However, changes in soil water …

In contrast to good knowledge of dissolved organic matter (DOM) adsorption on mineral
soils in temperate climate, the behavior of DOM in frozen mineral horizons located under …

Ice-rich yedoma-dominated landscapes store considerable amounts of organic carbon (C)
and nitrogen (N) and are vulnerable to degradation under climate warming. We investigate …

The large variety of the semi-automated methods in mapping the surface water bodies and
the frequent omission of ponds (< 10,000 m2) from permafrost regions inventories motivates …

Arctic plant productivity is often limited by low soil N availability. This has been attributed to
slow breakdown of N-containing polymers in litter and soil organic matter (SOM) into …