Abstract
The processes governing the transfer of gases across the air-sea interface have been reviewed by several authors (e.g. Bolin, 1960; Kanwisher, 1963; Broecker and Peng, 1974 Liss and Slater, 1976; Slinn et al.,l978). Basically, any net gas flux (F) across the interface must be driven by a concentration difference (ΔC) between air and surface water; the magnitude and direction of the flux being proportional to the numerical value and sign of ΔC, i.e.,
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Liss, P.S. (1983). Gas Transfer: Experiments and Geochemical Implications. In: Liss, P.S., Slinn, W.G.N. (eds) Air-Sea Exchange of Gases and Particles. NATO ASI Series, vol 108. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7169-1_5
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