Abstract
In order to obtain field data of ocean-atmosphere gas transfer coefficients, it is preferable to measure the interfacial gas flux in the air rather than in the water. This approach has been reported in the literature for CO2. However, it is shown here that 222Rn and methyliodide, CH3I, may be more suitable gases for air-side flux measurements.
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Roether, W. Field measurement of air-sea gas transfer: A methodical search. Boundary-Layer Meteorol 27, 97–103 (1983). https://doi.org/10.1007/BF00119974
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DOI: https://doi.org/10.1007/BF00119974