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- W2367492031 abstract "In this paper, based on the global warming characteristics, an ideal numerical experiment plan is designed, and a Boussinesq POP ocean model and a modified non-Boussinesq POP ocean model are used to quantitatively discuss the errors of Boussinesq approximation in ocean models. It is shown from the computation results that under the thermodynamic circulation condition by heating, the horizontal sea level rise distribution is basically uniform, and under the given initial and boundary conditions, the sea level error due to Boussinesq approximation can be as high as 59%, the sea surface height at the heat source center in Boussinesq model is much smaller than that in non-Boussinesq model, and there is false sea surface height fall around the heat source; under the thermohaline circulation condition by heating, the computed latitudinally and longitudinally vertical circulations are falsely strengthened due to Boussinesq approximation although this error is only about 1%; on the assumption of Boussinesq approximation, the error of vertically-integrated longitudinal heat flux at the equator is one-order greater than that of mass flux, the vertical distributions of air pressure gradient work calculated by non-Boussinesq model are fluctuating in water depths of greater than 3 000 m, but those calculated by Boussinesq model are basically uniform in water depths of greater than 3 000 m, and the error of Boussinesq approximation is more than 10%." @default.
- W2367492031 created "2016-06-24" @default.
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- W2367492031 date "2005-01-01" @default.
- W2367492031 modified "2023-09-23" @default.
- W2367492031 title "On the Errors of Boussinesq Approximation in Ocean Models" @default.
- W2367492031 hasPublicationYear "2005" @default.
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