On which timescales do gas transfer velocities control North Atlantic CO 2 flux variability?

The North Atlantic is an important basin for the global ocean's uptake of anthropogenic and natural carbon dioxide (CO 2 ), but the mechanisms controlling this carbon flux are not fully understood. The air‐sea flux of CO 2 , F , is the product of a gas transfer velocity, k , the air‐sea CO 2 concentration gradient, Δ p CO 2 , and the temperature‐ and salinity‐dependent solubility coefficient, α . k is difficult to constrain, representing the dominant uncertainty in F on short (instantaneous to interannual) timescales. Previous work shows that in the North Atlantic, Δ p CO 2 and k both contribute significantly to interannual F variability but that k is unimportant for multidecadal variability. On some timescale between interannual and multidecadal, gas transfer velocity variability and its associated uncertainty become negligible. Here we quantify this critical timescale for the first time. Using an ocean model, we determine the importance of k , Δ p CO 2 , and α on a range of timescales. On interannual and shorter timescales, both Δ p CO 2 and k are important controls on F . In contrast, pentadal to multidecadal North Atlantic flux variability is driven almost entirely by Δ p CO 2 ; k contributes less than 25%. Finally, we explore how accurately one can estimate North Atlantic F without a knowledge of nonseasonal k variability, finding it possible for interannual and longer timescales. These findings suggest that continued efforts to better constrain gas transfer velocities are necessary to quantify interannual variability in the North Atlantic carbon sink. However, uncertainty in k variability is unlikely to limit the accuracy of estimates of longer‐term flux variability. Global ocean carbon flux variability is simulated in a general circulation model Concentration gradient and transfer velocity control interannual flux variability Gas transfer velocity does not control pentadal North Atlantic flux variability