The main paths by which matter is transported between the shore of Admiralty Bay and the coastal and shelf waters are discussed in terms of trophic relations, physical forces, and fluctuations over long time scales and climatic changes.
Simple formula for computing irradiance attenuation in the Gulf of Gdansk waters in a func-tion of chlorophyll a concentration is obtained on the basis of field data. In its derivation, the relationship between Secchi depth and diffuse attenuation coefficient of visible irradiance was applied.
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