Abstract
Flows in natural fluid layers are often forced simultaneously at scales smaller and much larger than the depth. For example, the Earth’s atmospheric flows are powered by gradients of solar heating: vertical gradients cause three-dimensional (3D) convection whereas horizontal gradients drive planetary scale flows. Nonlinear interactions spread energy over scales1,2. The question is whether intermediate scales obtain their energy from a large-scale 2D flow or from a small-scale 3D turbulence. The paradox is that 2D flows do not transfer energy downscale whereas 3D turbulence does not support an upscale transfer. Here we demonstrate experimentally how a large-scale vortex and small-scale turbulence conspire to provide for an upscale energy cascade in thick layers. We show that a strong planar vortex suppresses vertical motions, thus facilitating an upscale energy cascade. In a bounded system, spectral condensation into a box-size vortex provides for a self-organized planar flow that secures an upscale energy transfer.
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Acknowledgements
This work was supported by the Australian Research Council’s Discovery Projects funding scheme (DP0881544) and by the Minerva Foundation and the Israeli Science Foundation.
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H.X., D.B. and M.S. designed and performed experiments; H.X. and D.B. analysed the data. M.S. and G.F. wrote the paper. All authors discussed and edited the manuscript.
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Xia, H., Byrne, D., Falkovich, G. et al. Upscale energy transfer in thick turbulent fluid layers. Nature Phys 7, 321–324 (2011). https://doi.org/10.1038/nphys1910
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DOI: https://doi.org/10.1038/nphys1910
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