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Titlebook: Air-Sea Exchange of Gases and Particles; Peter S. Liss,W. George N. Slinn Book 1983 D. Reidel Publishing Company, Dordrecht, Holland 1983

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https://doi.org/10.1007/978-3-322-93717-9roecker 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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978-94-009-7171-4D. Reidel Publishing Company, Dordrecht, Holland 1983
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https://doi.org/10.1007/978-3-642-91419-5An overview of such a complex system is necessarily incomplete. Emphasis is on such processes which relate more or less directly to the transport of gases and particles. The treatment in the introductory chapters on meteorology and physical oceanography is descriptive rather than deductive.
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