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Copy file name to clipboardExpand all lines: docs/src/modules/barotropicqgql.md
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- Constantinou, N. C., Farrell, B. F., and Ioannou, P. J. (2014). [Emergence and equilibration of jets in beta-plane turbulence: applications of Stochastic Structural Stability Theory.](http://doi.org/10.1175/JAS-D-13-076.1)*J. Atmos. Sci.*, **71 (5)**, 1818-1842.
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As in the [BarotropicQG module](barotropicqg.md), the flow is obtained through a streamfunction $\psi$ as $(u, v) = (-\partial_y\psi, \partial_x\psi)$. All flow fields can be obtained from the quasi-geostrophic potential vorticity (QGPV). Here the QGPV is
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As in the [SingleLayerQG module](singlelayerqg.md), the flow is obtained through a streamfunction $\psi$ as $(u, v) = (-\partial_y\psi, \partial_x\psi)$. All flow fields can be obtained from the quasi-geostrophic potential vorticity (QGPV). Here the QGPV is
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$$\underbrace{f_0 + \beta y}_{\text{planetary PV}} + \underbrace{(\partial_x v
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