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    Saline component of the buoyancy production 〈wS〉 and its components as a function of the parameter μ, where μ = 0 denotes the model with the total salt flux prescribed, whereas at μ = 1 the zonally averaged overturning component is prescribed (see Fig. 4). Note that an increase in 〈wS〉 corresponds to an increase in the weakening effect of salinity on the circulation strength (a decrease in 〈wB〉).

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CORRIGENDUM

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The corresponding author has reported that an alien illustration appeared in place of the correct illustration in Fig. 11 on page 2279 of the article “Impact of interbasin exchange on the Atlantic overturning circulation” by Wilbert Weijer, Wilhelmus P. M. De Ruijter, Henk A. Dijkstra, and Peter Jan van Leeuwen in the September 1999 Journal of Physical Oceanography, Vol. 29, No. 9, 2266–2284. The correct Fig 11, including the caption, appears as follows:

Fig. 11.
Fig. 11.

Saline component of the buoyancy production 〈wS〉 and its components as a function of the parameter μ, where μ = 0 denotes the model with the total salt flux prescribed, whereas at μ = 1 the zonally averaged overturning component is prescribed (see Fig. 4). Note that an increase in 〈wS〉 corresponds to an increase in the weakening effect of salinity on the circulation strength (a decrease in 〈wB〉).

Citation: Journal of Physical Oceanography 29, 12; 10.1175/1520-0485(1999)029<3185:C>2.0.CO;2

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