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Turbulence in a Fluid Stratified by a High Prandtl-Number Scalar

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Sustained Simulation Performance 2017

Abstract

Turbulence in the fluid stratified by a high Prandtl-number (P r) scalar such as heat (P r = 7) or salinity (P r = 700) has been simulated by direct numerical simulations, using 40963 grid points. Computations have been performed using the 1024 nodes of NEC SX-ACE, which have enabled us to resolve the smallest scale of salinity fluctuations \(\sqrt{ 700}(\sim 26)\) times smaller than the smallest eddy size. In our simulations, buoyancy initially affects only the large scale motions, and the k āˆ’1 spectrum predicted by Batchelor (J. Fluid Mech. 5:113ā€“133, 1959) for a passive scalar could be observed in the spectrum of potential energy, i.e. the salinity fluctuations. However, as time proceeds, the buoyancy affects the smaller-scale motions, and the salinity fluctuations begin to show a unique spatially localised structure. At the same time, there appears a flat spectrum ( āˆ k 0) instead of the k āˆ’1 spectrum. The localised structure and the flat spectrum could be observed only for the salinity (P r = 700) and not for heat (P r = 7).

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Acknowledgements

This research used computational resources of the HPCI system provided by Tohoku University through the HPCI System Research Project (Project ID: hp160108), and the Earth Simulator at the Japan Agency for Marine Earth Science and Technology.

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Correspondence to Hideshi Hanazaki .

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Okino, S., Hanazaki, H. (2017). Turbulence in a Fluid Stratified by a High Prandtl-Number Scalar. In: Resch, M., Bez, W., Focht, E., Gienger, M., Kobayashi, H. (eds) Sustained Simulation Performance 2017 . Springer, Cham. https://doi.org/10.1007/978-3-319-66896-3_7

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