While in T1–T3 all MHs had mean salinities >34 psu, there was a decreasing trend in salinity in the transects T4–T6, indicating a shift from North Sea to coastal water (Lee, 1980 ).
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While in T1–T3 all MHs had mean salinities >34 psu, there was a decreasing trend in salinity in the transects T4–T6, indicating a shift from North Sea to coastal water (Lee, 1980 ).