The formation, growth and drainage of lakes in Arctic and boreal lowland permafrost regions
influence landscape and ecosystem processes. These lake and drained lake basin (L-DLB) …

Significant progress in permafrost carbon science made over the past decades include the
identification of vast permafrost carbon stocks, the development of new pan‐Arctic …

Methane emissions from boreal and arctic wetlands, lakes, and rivers are expected to
increase in response to warming and associated permafrost thaw. However, the lack of …

Climate warming threatens to destabilize vast northern permafrost areas, potentially
releasing large quantities of organic carbon that could further disrupt the climate. Here we …

The contribution from northern high latitude wetlands are a major uncertainty in the
atmospheric methane (CH 4) budget throughout the Holocene. We reconstructed CH 4 …

Thermokarst lake formation accelerates permafrost degradation due to climate warming,
thereby releasing significant amounts of carbon into the atmosphere, complicating …

Climate-driven permafrost thaw can release ancient carbon to the atmosphere, begetting
further warming in a positive feedback loop. Polar ice core data and young radiocarbon …

Many scientific fields show great interest in the extraction and processing of spatiotemporal
data, such as medicine with an emphasis on epidemiology and neurology, geology, social …

With permafrost thaw, significant amounts of organic carbon (OC) previously stored in frozen
deposits are unlocked and become potentially available for microbial mineralization. This is …

Lakes act as important sinks for inorganic and organic sediment components. However,
investigations of sedimentary carbon budgets within glacial lakes are currently absent from …