Submarine permafrost is perennially cryotic earth material that lies offshore. Most submarine
permafrost is relict terrestrial permafrost beneath the Arctic shelf seas, was inundated after …

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 …

We used a satellite-derived global daily sea surface temperature (SST) dataset with
resolution 0.25× 0.25∘ to analyze interannual changes in the Arctic Shelf seas from 2000 to …

We present an assessment of changes in the gas hydrates stability zone of the Arctic Ocean
associated with subsea permafrost conditions. To evaluate the formation and dissociation of …

The response of permafrost to marine submergence can vary between ice‐rich late
Pleistocene deposits and the thermokarst basins that thawed out during the Holocene. We …

The sensitivity of seafloor temperature TB to the warming of surface air temperature T a is
examined for 1850–2300, based on simulations with five models from the Coupled Models …

As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and,
eventually, integrates them into subsea permafrost. Lagoons represent the first stage of a …

The Lena River plume significantly affects the thermohaline, optical and chemical properties
of the eastern Arctic seas. We use sea surface salinity (SSS), temperature (SST), and …

Аннотация Проанализировано влияние засоления на состояние затопленных морем
многолетнемёрзлых толщ шельфа моря Лаптевых. Результаты моделирования …

The simulations with SMILES (the Sediment Model Invented for Long-tErm Simulations) for
100 kyr in the future driven by the output of an Earth System Model with internally calculated …