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Stratification-dependent enstrophy-controlled regime in geostrophic turbulence

Abstract:
We experimentally measure geostrophic turbulence in a rotating, differentially heated fluid annulus, which is bounded by convectively driven warm and cold flows at the outer and inner boundaries, respectively. The horizontal kinetic energy spectra exhibit a range at low wavenumber which scales as 𝑘−3, where k denotes the horizontal wavenumber, with spectral amplitude that correlates with the square of the Brunt–Vaisala frequency at the same heights as the velocity measurements. The observed turbulent state exhibits a forward enstrophy cascade across all scales along with bidirectional energy transfer, which is evidenced by a reversal in the sign of the spectral energy flux at a scale proportional to the internal Rossby radius of deformation. These findings highlight the role of baroclinic instability in shaping the distribution of energy across scales with implications for synoptic-scale turbulent flows near Earth’s tropopause.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1103/n2nj-dg5r

Authors

More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
ORCID:
0000-0001-5040-3543


Publisher:
American Physical Society
Journal:
Physical Review Letters More from this journal
Volume:
136
Article number:
114101
Publication date:
2026-03-20
Acceptance date:
2026-02-10
DOI:
EISSN:
1079-7114
ISSN:
0031-9007


Language:
English
Pubs id:
2381344
Local pid:
pubs:2381344
Deposit date:
2026-02-25
ARK identifier:

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