In glacier forefields, the chronosequence approach is used to investigate ecological,
biogeochemical and physical features of autogenic successional change as a function of …

Land cover responses to climate change must be quantified for understanding Arctic climate,
managing Arctic water resources, maintaining the health and livelihoods of Arctic societies …

On‐going shrinkage of Greenland's icecap, permafrost thaw, and changes in precipitation
are exposing its landscapes to erosion and remobilization of ancient organic carbon (OC) …

Soil organic carbon (SOC) in Arctic coastal polygonal tundra is vulnerable to climate
change, especially in soils with occurrence of large amounts of ground ice. Pan-arctic …

Large amounts of soil organic carbon (SOC) have accumulated over thousands of years in
the northern permafrost regions. However, the SOC accumulation rates and the effects of …

In this study we assess the total storage, landscape distribution, and vertical partitioning of
soil organic carbon (SOC) stocks on the Brøgger Peninsula, Svalbard. This type of high …

In the Arctic, climate changes contribute to enhanced mobilization of organic matter in
streams. Microbial extracellular enzymes are important mediators of stream organic matter …

Climate change is causing drastic landscape changes in the Arctic, but how these changes
modify stream biogeochemistry is not clear yet. We examined how catchment properties …

Nigeria generally has a warm climate all year round, with marked differences between dry
and wet seasons. The wet season is normally from April to October, while the dry season is …

As Arctic regions warm rapidly, it is unclear whether high‐latitude soil carbon (C) will
decrease or increase. Predicting future dynamics of Arctic soil C stocks requires a better …