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

• Published in: Geophysical Research Letters
• Main Authors: DeGrandpre, M. D., Körtzinger, Arne, Send, Uwe, Wallace, Douglas W.R., Bellerby, R. G. J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: AGU (American Geophysical Union) 2006
• Subjects: Labrador Sea
• Online Access: https://oceanrep.geomar.de/id/eprint/7278/; https://oceanrep.geomar.de/id/eprint/7278/1/DeGrandpre_et_al-2006-Geophysical_Research_Letters.pdf; https://doi.org/10.1029/2006GL026881

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-series 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 CO2 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.