A major surface circulation feature of the Arctic Ocean is the Transpolar Drift (TPD), a current
that transports river‐influenced shelf water from the Laptev and East Siberian Seas toward …

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 …

Climate change affects the Arctic with regards to permafrost thaw, sea-ice melt, alterations to
the freshwater budget and increased export of terrestrial material to the Arctic Ocean. The …

Abstract As the Arctic Ocean (AO) is increasingly altered by anthropogenic climate change, it
is critical that we accurately assess ongoing changes in its capacity to support marine life …

Climate-change driven increases in temperature and precipitation are leading to increased
discharge of freshwater and terrestrial material to Arctic coastal ecosystems. These inputs …

Eastern Fram Strait and the shelf slope region north of Svalbard is dominated by the
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …

Global warming is not often discussed in the context of light availability within the water
column. However, the light regimes in the Arctic Ocean are controlled by three factors that …

How much light is available for biological processes during Polar Night? This question
appears simple enough. But the reality is that conventional light sensors for measuring …

Abstract The Arctic Ocean is rapidly changing from thicker multiyear to thinner first‐year ice
cover, with significant consequences for radiative transfer through the ice pack and light …

The marginal sea ice zone has been identified as a source of different climate-active gases
to the atmosphere due to its unique biogeochemistry. However, it remains highly …