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27
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3543075618
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note
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-1) (2, 22, 23) was used for a Schmidt number Sc = 600 (24), which is a typical value for a moderately turbulent river (25).
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28
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3543103660
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note
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2 gradient (27), is in good agreement with those reported for rivers (25). It should be pointed out that, if wind becomes predominant, actual efflux would be higher than our estimate.
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29
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3543108318
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note
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We thank the crews and technicians who were involved in the numerous cruises, R. Wollast and two anonymous referees for helpful comments on a previous version of this manuscript, and A. Pollentier, J. Backers, and A. Peliz for providing salinity and temperature data. Funded by the Fonds National de la Recherche Scientifique (FNRS, Belgium), with which the senior author is a research associate, and the European Union [Marine Science and Technology (MAST) and Environment and Climate programs]. This is a contribution to the European Land Ocean Interactions Studies (ELOISE) Programme (publication number 037) in the framework of the Biogas Transfer in Estuaries (BIOGEST) project carried out under contract ENV4-CT96-0213.
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