Table 1.
Location | Date | Non-purgeable DOC in seawater (μM C) | EDOC* (μM C) | k600 | Wind speed (m s−1) | GOC/H′ in seawater (μM C) | Air-sea OC flux** (mmol C m−2 d−1) |
---|---|---|---|---|---|---|---|
Mediterranean Sea (A) | 04-Jun-06 | 71.8 | 24 | 1.23 | 4.5 | 51 | −25.4 |
NE Subtropical Atlantic (B) | 21-Aug-06 | 79 | 14 | 3.8 | 8 | 19 | −14.18 |
NE Subtropical Atlantic (C) | 25-Aug-06 | 86.23 | 22 | 3.8 | 8 | 35 | −36.86 |
NE Subtropical Atlantic (D) | 03-Feb-07 | 68.3 | 73 | 4.29 | 8.5 | 88 | −47.93 |
NE Subtropical Atlantic (E) | 19-Feb-07 | 82.9 | 18 | 2.92 | 7 | 28 | −21.81 |
Arctic Ocean (F) | 05-Jul-07 | 94.3 | 35 | 0.98 | 4 | 39 | −1.62 |
Arctic Ocean (G) | 20-Jul-07 | 91.3 | 0 | 2.16 | 6 | 5 | −4.21 |
82.9 | 22 | 2.92 | 7 | 35 | −18 |
EDOC is defined as the concentration of organic carbon in surface water that can be exchanged with the atmosphere.
Negative values indicate net inputs from the atmosphere into the ocean. Net fluxes of OC calculated using alternative parameterisations of k600 are reported as Supplementary Material.