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What is a small enough temperature difference to make the boussinesq assumption? 


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The Boussinesq approximation is commonly used in natural convection problems, but its validity is limited to small temperature differences. The exact threshold for a "small enough" temperature difference varies depending on the specific problem being studied. However, some papers provide insights into this. Manela and Frankel suggest that for small temperature differences, the Boussinesq approximation holds when based on a modified Rayleigh number incorporating the potential-temperature gradient . El-Gendi and Aly mention that using the Boussinesq approximation, the temperature difference should be less than 28.6 K . Asai and Nakasuji indicate that the Boussinesq approximation is applicable when the Mach number, the relative range of the potential temperature, and the ratio of the depth of the layer to that of the isentropic atmosphere are much smaller than unity . Therefore, the specific temperature difference that qualifies as "small enough" depends on the context and the specific problem being analyzed.

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The paper does not provide a specific value for the temperature difference that is considered small enough to make the Boussinesq assumption.
The paper does not provide information about the specific temperature difference required to make the Boussinesq assumption.
The paper states that the temperature difference should be less than 28.6 K to make the Boussinesq approximation.
The paper does not provide a specific value for the temperature difference that is considered small enough to make the Boussinesq assumption.

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