Abstract The western Fram Strait is the only deep-water gateway connecting the Arctic
Ocean and North Atlantic. Consequently, today, the western Fram Strait and the Northeast …

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 …

Abstract The Arctic Ocean features extreme seasonal differences in daylight, temperature,
ice cover, and mixed layer depth. However, the diversity and ecology of microbes across …

Carbohydrates are chemically and structurally diverse, represent a substantial fraction of
marine organic matter and are key substrates for heterotrophic microbes. Studies on …

The Little Ice Age (LIA) was one of the coldest periods of the postglacial period in the
Northern Hemisphere. Although there is increasing evidence that this time interval was …

We report on stable oxygen and carbon isotope data obtained on two different morphotypes
of polar planktic foraminifers, ie, fully encrusted and minor encrusted Neogloboquadrina …

The hydrography of the Arctic Seas is being altered by ongoing climate change, with knock‐
on effects to nutrient dynamics and primary production. As the major pathway of exchange …

Sea ice modulates the energy exchange between the atmosphere and the ocean through its
kinematics. Marginal ice zone (MIZ) dynamics are complex and are not well resolved in …

Abstract The Arctic Ocean is considered a source of micronutrients to the Nordic Seas and
the North Atlantic Ocean through the gateway of Fram Strait (FS). However, there is a paucity …

Abstract The Fram Strait is the only deep connection between the Arctic and Atlantic Oceans.
The main water and mercury (Hg) fluxes between these oceans occur via the Fram Strait …