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Diffusion-Free Scaling in Rotating Spherical Rayleigh–Bénard Convection
Open Access
Geophysical Research Letters
48
, e2021GL095017 (
2021
)
Authors
Guiquan Wang
Luca Santelli
Detlef Lohse
Roberto Verzicco
Richard Stevens
BibTeΧ
@article{https://doi.org/10.1029/2021GL095017, author = {Wang, Guiquan and Santelli, Luca and Lohse, Detlef and Verzicco, Roberto and Stevens, Richard J. A. M.}, title = {Diffusion-Free Scaling in Rotating Spherical Rayleigh-Bénard Convection}, journal = {Geophysical Research Letters}, volume = {48}, number = {20}, pages = {e2021GL095017}, keywords = {Thermal convection, spherical shell, rapidly rotating, diffusion-free scaling}, doi = {https://doi.org/10.1029/2021GL095017}, url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021GL095017}, eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL095017}, note = {e2021GL095017 2021GL095017}, abstract = {Abstract Direct numerical simulations are employed to reveal three distinctly different flow regions in rotating spherical Rayleigh-Bénard convection. In the high-latitude region vertical (parallel to the axis of rotation) convective columns are generated between the hot inner and the cold outer sphere. The mid-latitude region is dominated by vertically aligned convective columns formed between the Northern and Southern hemispheres of the outer sphere. The diffusion-free scaling, which indicates bulk-dominated convection, originates from this mid-latitude region. In the equator region , the vortices are affected by the outer spherical boundary and are much shorter than in region .}, year = {2021} }
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