========================================= Model equations ========================================= Here we provide that governing equations of the two-layer QG channel model. Governing equations ~~~~~~~~~~~~~~~~~~~~~~~~~ The governing equations for the present two-layer QG model are .. math:: \begin{equation} \partial_{t} q_{1} + \mathrm{J} (\psi_{1}, \, q_{1} ) = \kappa_\mathrm{T} \left ( \frac{\psi_{1} - \psi_{2}}{2} - \tau_\mathrm{eq.} \right ) - \nu \nabla^4 q_{1} \end{equation} .. math:: \begin{equation} \partial_{t} q_{2} + \mathrm{J} (\psi_{2}, \, q_{2} ) = - \kappa_\mathrm{T} \left ( \frac{\psi_{1} - \psi_{2}}{2} - \tau_\mathrm{eq.} \right ) - \mu \nabla^2 \psi_{2} - \nu \nabla^4 q_{2} \end{equation} Linear friction in the lower layer has the coefficient :math:`\mu`, with dimensions of inverse time. Hyperviscosity is applied to the streamfunction in both layers and has the coefficient :math:`\nu` with dimensions of :math:`\mathrm{L}^{4} \mathrm{T}`. :math:`\kappa_\mathrm{T}` is an inverse time scale for damping the baroclinic flow to the background streamfunction, :math:`\tau_\mathrm{eq.}`. We now describe a specific example.