Abstract :
[en] High biological activity causes a distinct seasonality of surface water pH in the North
Sea, which is a strong sink for atmospheric CO
2
via an effective shelf pump. The intimate
connection between the North Sea and the North Atlantic Ocean suggests that the variability
of the CO
2
system of the North Atlantic Ocean may, in part, be responsible for the observed
variability of pH and CO
2
in the North Sea. In this work, we demonstrate the role of the
North Atlantic Oscillation (NAO), the dominant climate mode for the North Atlantic, in
governing this variability. Based on three extensive observational records covering the
relevant levels of the NAO index, we provide evidence that the North Sea pH and CO
2
system strongly responds to external and internal expressions of the NAO. Under positive
NAO, the higher rates of in
fl
ow of water from the North Atlantic Ocean and the Baltic
out
fl
ow lead to a strengthened north-south biogeochemical divide. The limited mixing
between the north and south leads to a steeper gradient in pH and partial pressure of CO
2
(pCO
2
) between the two regions in the productive period. This is exacerbated further when
coinciding with higher sea surface temperature, which concentrates the net community
production in the north through shallower strati
fi
cation. These effects can be obscured by
changing properties of the constituent North Sea water masses, which are also in
fl
uenced by
NAO. Our results highlight the importance of examining interannual trends in the North Sea
CO
2
system with consideration of the NAO state
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