Phytoplankton production in the coastal water is to a large degree influenced by local hydrologic and meteorological factors, including fresh water runoff, wind mixing, tidal regime, as well as ice melting in the coastal areas. As for the open ocean the annual phytoplankton cycle could be divided into phases (winter, spring, summer, and autumn) as for the open areas. Along the Barents Sea coastal line there is large variation in the onset of the different phases along the Russian and Norwegian coast.






