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

Climate change is an existential threat to the vast global permafrost domain. The diverse
human cultures, ecological communities, and biogeochemical cycles of this tenth of the …

The CryoGrid community model is a flexible toolbox for simulating the ground thermal
regime and the ice–water balance for permafrost and glaciers, extending a well-established …

Based on a regional ice-ocean model, we simulated the state of the water masses of the
Arctic Ocean to analyze the transport of dissolved methane on the Arctic shelves. From 1970 …

The Russian sector of the arctic shelf is the longest in the world. Quite a lot of places of
massive discharge of bubble methane from the seabed into the water column and further …

Several studies have investigated changes in microbial community composition in thawing
permafrost landscapes, but microbial assemblages in the transient ecosystems of the Arctic …

Sea level rise and coastal erosion have inundated large areas of Arctic permafrost.
Submergence by warm and saline waters increases the rate of inundated permafrost thaw …

Arctic permafrost coasts, affected by rising sea levels and increasing coastal erosion in a
warming climate, undergo significant changes. Simulating how permafrost is impacted by …

Subsea permafrost stability is the key to whether pre-performed methane sequestered in
hydrate deposits escapes to the overlying strata. By making use of the 1D numerical …

The Arctic has experienced rapid change associated with warming since the 1970s. The
rapid retreat of the terrestrial cryosphere can release a large amount greenhouse gas from …