engleski

Two different northern Adriatic winter oceanographic types

It has been observed that two types (A and B) of winter oceanographic conditions can occur in the northern Adriatic. The difference between the eastern and western parts bottom layer density distinguishes the two winter types. We intend to present a precise definition of the two types and introduce a third winter type (C). A and B types differ in hydrographic (temperature and salinity), dynamic (geostrophic currents distributions), chemical (total inorganic nitrogen and phosphorous) and biological (phytoplankton) parameters.

Adriatic Sea ; Circulation ; Nutrients ; Phytoplankton ; Po Delta

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