A numerical scheme to calculate temperature and salinity dependent air-water transfer velocities for any gas
The ocean-atmosphere flux of a gas can be calculated from its measured or estimated concentration gradient across the air-sea interface and the transfer velocity (a term representing the conductivity of the layers either side of the interface with respect to the gas of interest). Traditionally the t...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2010-10-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/6/913/2010/os-6-913-2010.pdf |