Our knowledge on permafrost carbon (C) cycle is crucial for understanding its feedback to
climate warming and developing nature-based solutions for mitigating climate change. To …

Atmospheric methane (CH 4) concentrations have gone through rapid changes since the
last deglaciation; however, the reasons for abrupt increases around 14,700 and 11,600 …

Climate-sensitive northern cryosphere inland waters emit greenhouse gases (GHGs) into
the atmosphere, yet their total emissions remain poorly constrained. We present a data …

Basic inventory is required for proper understanding and utilization of Earth's natural
resources, especially with increasing soil degradation and species loss. Soil carbon is newly …

Permafrost thaw in northern peatlands causes collapse of permafrost peat plateaus and
thermokarst bog development, with potential impacts on atmospheric greenhouse gas …

Large stocks of soil carbon (C) and nitrogen (N) in northern permafrost soils are vulnerable
to remobilization under climate change. However, there are large uncertainties in present …

Land surface temperature (LST) has gained increased attention in cryospheric research.
While various global satellite LST products are available, none of them is specially designed …

Drained lake basins (DLBs) are dominant features in lowland permafrost landscapes of the
Arctic. Here, we present a novel approach describing and quantifying the succession …

Warming in permafrost regions stimulates carbon (C) release through decomposition, but
increasing atmospheric CO2 and available soil nitrogen enhance plant productivity at the …

Research in geocryology is currently principally concerned with the effects of climate change
on permafrost terrain. The motivations for most of the research are (1) quantification of the …