Abstract.The consequences of the following episodic phenomena for the pelagic‐benthic coupling in the Nordic Seas are illustrated: (1) Advection of water masses between fjords and shelf environments, (2) freshwater run‐off and vertical stability, (3) dynamics of the marginal ice zone in the central and northern Barents Sea and the Polar Ocean, (4) drift patterns of sinking particles along the North Norwegian coast, (5) advection of zooplankton into subarctic fjords and the southern Barents Sea, zooplankton overwintering and composition, and (6) transport of organic particulate matter from the Barents Sea shelf. It is shown that physical processes in the north‐eastern North Atlantic and Polar Ocean can be strongly variable on time scales of days to decades. They have a significant influence on the dynamics of pelagic‐benthic coupling. The physical oceanography influences the vertical and horizontal particle flux not only directly (mixing, advection, up‐ and down‐welling), but also indirectly through its impact on the biota (for example radiation, wind, ice cover, freshwater run‐off and overwintering, advection and retention of zooplankton). Understanding pelagic‐benthic coupling at high latitudes depends even more on a best possible understanding of the physical oceanography and the time scales involved
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