The cryosphere is an important component of the global climate system. Cryospheric
components are sensitive to climate warming, and changes in the cryosphere can lead to …

The pattern of occurrence and recent changes in the distribution of macrobenthic organisms
in fjordic and coastal (nearshore) Arctic waters are reviewed and future changes are …

Permafrost coasts in the Arctic are susceptible to a variety of changing environmental factors
all of which currently point to increasing coastal erosion rates and mass fluxes of sediment …

In the future, Earth will be warmer, precipitation events will be more extreme, global mean
sea level will rise, and many arid and semiarid regions will be drier. Human modifications of …

Storm event statistics for the open-water season (June–October) were extracted from the
terrestrial-based observational record throughout the circumpolar coastal regime over the …

Permafrost coasts make up to 34 per cent of the world's coastlines. Erosion of these coasts
currently averages 0.5 ma‐1, which is similar to or greater than rates observed in temperate …

Rocky littoral macroorganisms that live between the high and low water marks were
sampled in the summers of 1988 and 2007–2008 in Hornsund Fjord and along the adjacent …

Sediments covering Arctic continental shelves are uniquely impacted by ice processes.
Delivery of sediments is generally limited to the summer, when rivers are ice free, permafrost …

Abstract The North Pacific and Bering Sea regions represent loci of cyclogenesis and storm
track activity. In this paper climatological properties of extratropical storms in the North …

The southeast coastline of the Barents Sea in the area of the Varandey settlement is
characterized by warm permafrost. Coastal studies conducted since the early 1980s have …