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<p><strong>Abstract.</strong> The estimation of sea–air CO<sub>2</sub> fluxes is largely dependent on wind speed through the gas transfer velocity parameterization. In this paper, we quantify uncertainties in the estimation of the CO<sub>2</sub> uptake in the Bay of Biscay resulting from the use of different sources of wind speed such as three different global reanalysis meteorological models (NCEP/NCAR 1, NCEP/DOE 2 and ERA-Interim), one high-resolution regional forecast model (HIRLAM-AEMet),doi:10.5194/bg-10-2993-2013 fatcat:uqaojjilyvhajj5nooacs5yu6q