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We show the vertical distributions of temperature, salinity, nutrients, oxygen, CO 2 fugacity (fCO 2 ), pH and chlorophyll-a at the end of the winter 1984 in the northeast sector of the Atlantic Ocean between 40°N and 47°N. The intense vertical mixing due to winter cooling resulting in homogeneous water column layers as deep as 300 m at 47°N and, getting shallower further south to...
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