Abstract Changes in the Arctic atmosphere, cryosphere and Ocean are drastically altering
the dynamics of phytoplankton, the base of marine ecosystems. This Review addresses four …

Climate change impacts are pronounced at high latitudes, where warming, reduced sea-ice-
cover, and ocean acidification affect marine ecosystems. We review climate change impacts …

Historically, sea ice loss in the Arctic Ocean has promoted increased phytoplankton primary
production because of the greater open water area and a longer growing season. However …

The Arctic marine biome, shrinking with increasing temperature and receding sea-ice cover,
is tightly connected to lower latitudes through the North Atlantic. By flowing northward …

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 …

Temporal and spatial dynamics of phytoplankton and zooplankton in the Barents Sea have
been investigated during the last three decades using remote sensing and in situ …

Abstract The Arctic Ocean and its surrounding shelf seas are warming much faster than the
global average, which potentially opens up new distribution areas for temperate‐origin …

As a cooling machine of the Arctic Ocean, the Barents Sea releases most of the incoming
ocean heat originating from the North Atlantic. The related air-sea heat exchange plays a …

The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable
evidence of the rapid changes occurring in this region. Understanding the past variability of …

Marine heatwaves (MHWs) can potentially alter ocean ecosystems with far-reaching
ecological and socio-economic consequences. This study investigates the spatiotemporal …