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Characterizing Regimes of Atmospheric Circulation in Terms of Their Global Superrotation
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Characterizing Regimes of Atmospheric Circulation in Terms of Their Global Superrotation
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Journal Article
Characterizing Regimes of Atmospheric Circulation in Terms of Their Global Superrotation
2021
Overview
The global superrotation index S compares the integrated axial angular momentum of the atmosphere to that of a state of solid-body corotation with the underlying planet. The index S is similar to a zonal Rossby number, which suggests it may be a useful indicator of the circulation regime occupied by a planetary atmosphere. We investigate the utility of S for characterizing regimes of atmospheric circulation by running idealized Earthlike general circulation model experiments over a wide range of rotation rates Ω, 8Ω E to Ω E /512, where Ω E is Earth’s rotation rate, in both an axisymmetric and three-dimensional configuration. We compute S for each simulated circulation, and study the dependence of S on Ω. For all rotation rates considered, S is on the same order of magnitude in the 3D and axisymmetric experiments. For high rotation rates, S ≪ 1 and S ∝ Ω −2 , while at low rotation rates S ≈ 1/2 = constant. By considering the limiting behavior of theoretical models for S , we show how the value of S and its local dependence on Ω can be related to the circulation regime occupied by a planetary atmosphere. Indices of S ≪ 1 and S ∝ Ω −2 define a regime dominated by geostrophic thermal wind balance, and S ≈ 1/2 = constant defines a regime where the dynamics are characterized by conservation of angular momentum within a planetary-scale Hadley circulation. Indices of S ≫ 1 and S ∝ Ω −2 define an additional regime dominated by cyclostrophic balance and strong equatorial superrotation that is not realized in our simulations.
Publisher
American Meteorological Society
Subject
