Turbulent rotating convection to the extreme (TROCONVEX)
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Large-scale flows on Earth are forced by temperature differences and are affected by Earths rotation. Examples include the atmosphere and the flow in the liquid outer core. A laboratory experiment to study such systems necessarily has a finite size. Researchers investigate the effects of presence of sidewalls on the flows, to be able to better interpret results from these experiments. With this knowledge the translation from experiment to the large-scale natural flows can be performed more accurately.
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