Uptake and sequestration of atmospheric CO₂ in the Labrador Sea deep convection region

The Labrador Sea is an important area of deep water formation and is hypothesized to be a significant sink for atmospheric CO₂ to the deep ocean. Here we examine the dynamics of the CO₂ system in the Labrador Sea using time-serjes data obtained from instrumentation deployed on a mooring near the former Ocean Weather Station Bravo. A 1-D model is used to determine the air-sea CO₂ uptake and penetration of the CO ₂ into intermediate waters. The results support that mixed-layer pCO₂ remained undersaturated throughout most of the year, ranging from 220 μatm in mid-summer to 375 μatm in the late spring. Net community production in the summer offset the increase in pCO₂ expected from heating and air-sea uptake. In the fall and winter, cooling counterbalanced a predicted increase in pCO₂ from vertical convection and air-sea uptake. The predicted annual mean air to sea flux was 4.6 mol m^-2 yr^-1 resulting in an annual uptake of 0.011 ± 0.005 Pg C from the atmosphere within the convection region. In 2001, approximately half of the atmospheric CO₂ penetrated below 500 m due to deep convection.