SpringerImages - Simulated preindustrial minus 9–8 k anomaly map for the convection depth (m) in January

Simulated preindustrial minus 9–8 k anomaly map for the convection depth (m) in January

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Simulated preindustrial minus 9–8 k anomaly map for the convection depth (m) in January

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The long-term reduction in overturning circulation in the Nordic Seas is accompanied by a decrease in the convection depth south of Svalbard (Fig. 15 ).

First, our simulation shows a shallower deep convection (by more than 250 m, Fig. 15 ) and weakened overturning strength (by 0.5 Sv, Fig. 14 ) in the Nordic Seas, while it is enhanced in the Labrador Sea.

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