The Atlantic gateway to the Arctic Ocean is influenced by vigorous inflows of Atlantic Water.
The high-latitude impacts of these inflows have strengthened owing to climate change …

The Arctic has warmed dramatically in recent decades, with greatest temperature increases
observed in the northern Barents Sea. The warming signatures are not constrained to the …

Abstract Barents Sea Water (BSW) is formed from Atlantic Water that is cooled through
atmospheric heat loss and freshened through seasonal sea ice melt. In the eastern Barents …

Large‐scale patterns in species diversity and community composition are associated with
environmental gradients, but the implications of these patterns for food‐web structure are …

Abstract The Northeast Greenland shelf (NEGS) is a recipient of Polar Water (PW) from the
Arctic Ocean, Greenland Ice Sheet melt, and Atlantic Water (AW). Here, we compile …

The northern Barents Sea is a cold, seasonally ice-covered Arctic shelf sea region that has
experienced major warming and sea ice loss in recent decades. Here, a 2-year …

Glaciers in the Arctic have lost considerable mass during the last two decades. About a third
of the glaciers by area drains into the ocean, yet the mechanisms and drivers governing …

Copepods from the genus Calanus are crucial prey for fish, seabirds and mammals in the
Nordic and Barents Sea ecosystems. The objective of this study is to determine the …

We review recent trends and projected future physical and chemical changes under climate
change in transition zones between Arctic and Subarctic regions with a focus on the two …

The Barents Sea is one of the Polar regions where current climate and ecosystem change is
most pronounced. Here we review the current state of knowledge of the physical, chemical …