2020
DOI: 10.1103/physrevfluids.5.113501
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Laboratory exploration of heat transfer regimes in rapidly rotating turbulent convection

Abstract: DOI to the publisher's website. • The final author version and the galley proof are versions of the publication after peer review. • The final published version features the final layout of the paper including the volume, issue and page numbers. Link to publication General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal… Show more

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Cited by 33 publications
(101 citation statements)
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References 56 publications
(158 reference statements)
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“…For large Pr 2 we observe columns above the line Ra/Ra C ≈ 2 (Figure 2(b)). It is clear from DNS [78] and experiments [40,44] that the steep Nu(Ra) scaling is for columns, with exponent β increasing as E is reduced; β = 3.6 at E = 10 −7 is the steepest scaling reported so far [40]. The demarcation between regimes 2 and 3 (as inferred from heat transfer graphs) coincides with the transition between columns and plumes, hence the proposed terminology of columnar convection for regime 3.…”
Section: A Sketch Of the Geostrophic Regimementioning
confidence: 56%
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“…For large Pr 2 we observe columns above the line Ra/Ra C ≈ 2 (Figure 2(b)). It is clear from DNS [78] and experiments [40,44] that the steep Nu(Ra) scaling is for columns, with exponent β increasing as E is reduced; β = 3.6 at E = 10 −7 is the steepest scaling reported so far [40]. The demarcation between regimes 2 and 3 (as inferred from heat transfer graphs) coincides with the transition between columns and plumes, hence the proposed terminology of columnar convection for regime 3.…”
Section: A Sketch Of the Geostrophic Regimementioning
confidence: 56%
“…These four flow morphologies have also been found in DNS [78]. In many experiments these flow structures have also been identified using dye [82], shadowgraphy [59], passive tracers [5,40,44,83,84] and thermochromic liquid crystals [67,72]. They could also be identified in quantitative flow measurements using particle image velocimetry (PIV) [45,68,71,73,74,85] or 3D particle tracking velocimetry (PTV) [71].…”
Section: A Sketch Of the Geostrophic Regimementioning
confidence: 82%
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