Permafrost covers a quarter of the northern hemisphere land surface and contains twice the
amount of carbon that is currently present in the atmosphere. Future climate change is …

Recent studies have shown that climate change is impacting the inorganic chemical
characteristics of surface fresh water in permafrost areas and affecting aquatic ecosystems …

Thermokarst lakes are an important ecosystem component in permafrost terrains; therefore,
quantifying changes in these lakes is important for evaluating the water balance and carbon …

The Arctic is a water-rich region, with freshwater systems covering about 16% of the northern
permafrost landscape. Permafrost thaw creates new freshwater ecosystems, while at the …

Abstract The Western Siberia Lowland (WSL), the world's largest permafrost peatland, is of
importance for understanding the high-latitude carbon (C) cycle and its response to climate …

As high latitudes warm, vast stocks of carbon and nitrogen stored in permafrost will become
available for transport to aquatic ecosystems. While there is a growing understanding of the …

Analysis of organic and inorganic carbon (DOC and DIC, respectively), pH, Na, K, Ca, Mg,
Cl, SO 4 and Si in~ 100 large and small rivers (< 10 to≤ 150 000 km 2) of western Siberia …

The organic-carbon (OC) pool accumulated in Arctic permafrost (perennially frozen ground)
equals the carbon stored in the modern atmosphere. To give an idea of how Yedoma region …

On-going permafrost thaw in discontinuous permafrost regions produces significant amounts
of small permafrost subsidence and depressions, while large lakes are likely to drain into …

Towards a better understanding of trace element (TE) transport in permafrost-affected Earth
surface environments, we sampled∼ 60 large and small rivers (< 100 to≤ 150 000 km 2 …