Abstract
We consider a 2-layer quasi-geostrophic ocean model where the upper layer is forced by a steady Kolmogorov wind stress in a periodic channel domain, which allows to mathematically study the nonlinear development of the resulting flow. The model supports a steady parallel shear flow as a response to the wind stress. As the maximal velocity of the shear flow (equivalently the maximal amplitude of the wind forcing) exceeds a critical threshold, the zonal jet destabilizes due to baroclinic instability and we numerically demonstrate that a first transition occurs. We obtain reduced equations of the system using the formalism of dynamic transition theory and establish two scenarios which completely describe this first transition. The generic scenario is that a conjugate pair of modes loses stability and a Hopf bifurcation occurs as a result. Under an appropriate set of parameters describing related midlatitude oceanic flows, we show that this first transition is continuous: a supercritical Hopf bifurcation occurs and a stable time periodic solution bifurcates. We also investigate the case of double Hopf bifurcations which occur when four modes of the linear stability problem simultaneously destabilize the zonal jet. In this case, we prove that, in the relevant parameter regime, the flow exhibits a continuous transition accompanied by a bifurcated attractor homeomorphic to \(S^3\). The topological structure of this attractor is analyzed in detail and is shown to depend on the system parameters. In particular, this attractor contains (stable or unstable) time-periodic solutions and a quasi-periodic solution.
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The datasets generated during the current study are available from the corresponding author on reasonable request.
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Acknowledgements
The authors are grateful for two anonymous reviewers for their insightful comments. This work has been partially supported by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (Grant Agreement No. 810370). This study was also supported by a Ben May Center grant for theoretical and/or computational research.
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Appendices
Appendix A: Proof of Lemma 1 and Theorem 1
We first proceed with the proof of Lemma 1 For this, we denote the adjoint modes by
We denote the critical eigenmode and the critical eigenvalue by
We denote the bilinear operator \({\mathcal {G}}\) as
where \(G_{2}(u, v)\) is linear in each component. Let us define now
The center part of the solution is
where c.c. stands for complex conjugate of the terms before.
The evolution of z(t) near the onset of transition is obtained by the projection onto the critical mode \(\psi _c\).
where \(\varPhi \) is the center manifold function. We will obtain its quadratic approximation \(\varPhi _2\) given by
Here
denotes higher than n-th order terms in \(z, {\overline{z}}\).
Using notation (26), the reduced Eq. (28) can be written
To obtain a closed system, we need to approximate the center manifold function. The approximation of the center manifold in this case reads, see [30],
where \({\mathcal {L}} = \varPi _{s} {\mathcal {M}}^{-1} {\mathcal {N}}\) and \(\varPi _{s}\) is the projection on the stable space. Using formula (30), we obtain the following expansion of the center manifold (see also [5, Theorem 2])
Here
are the coefficients of the center manifold function.
We write (29) as (19), that is
which finishes the proof of Lemma 1.
Recalling the definition of \(G_s\) given in (26), the transition number P can then be written as
where
denotes the contribution of the zero-wavenumber (stable) modes \(\psi _{0, j}\) while
denotes the contribution of the modes \(\psi _{2m_{c}, j}\) on the transition number, respectively. The transition type depends on the real part of the transition number P. The proof of Theorem 1 follows from the standard Hopf bifurcation analysis of the reduced equation.
Appendix B: Proof of Lemma 2 and Theorem 2
As the reduction in the case of (18) is similar to the case of (17) given in the previous section, we will only mention the differences between these two cases. Under assumption (18), we write the center part of the solution as
where the first two critical modes are
with corresponding eigenvalues
Eq. (29) becomes the system
and the center manifold function (30) is replaced by
where \(\varPi _s\) denotes the projector onto the stable subspace.
Now, Eq. (36) becomes (21) with the coefficients defined below:
We note that the above coefficients contain only \(g_{i, j, k, l}\) for which \(i+j+k = l\). The expansion of the center manifold coefficients can be written more explicitly as (see also [5, Theorem 2])
Now we analyze Eq. (21) by first putting them in polar form
which yields
and
For the specific case of (22), Eq. (38) always admits the solutions which represent the periodic solutions
with respective eigenvalues
Also, Eq. (38) admits the following solution which represents a quasi-periodic solution
Since the Jacobian matrix of the right-hand side of (38) at the quasi-periodic solution has determinant
With this information, the transition scenarios summarized in Figs. 10 and 11 can be obtained by a standard analysis. To prove the claim on the bifurcation of an \(S^3\)-attractor, we need to prove that \((\rho _1, \rho _2) = (0, 0)\) is locally stable equilibrium of (38) at \(\varPsi = \varPsi _c\), that is when \({\text {Re}}(\sigma _1) = {\text {Re}}(\sigma _2) = 0\). In this case by assumption (22), from (38), we can obtain
which proves the claim.
Appendix C: Numerical treatment of the linear stability problem
To solve the eigenvalue problem numerically, we first plugin the ansatz
into the eigenvalue problem
to obtain
Here the linear operators \(\widetilde{{\mathcal {M}}}\) and \(\widetilde{{\mathcal {N}}}(y)\) are defined as
where
The eigenvalue problem (40) is supplemented with the following boundary conditions
We use Legendre–Galerkin method to discretize and solve (40) with boundary conditions (43). We refer to [31] for the details of the Legendre–Galerkin method and to [10] for its use in dynamical transition problems.
Let \(\{ L_{j} \}\) be the Legendre polynomials and consider compact combinations of the Legendre polynomials
with \(c_{jk}\) chosen so that \(f_{j}\) satisfy the boundary conditions (43), i.e.,
To discretize the eigenvalue problem, we plug
into (40) to obtain
Here
with \((f, g) = \int _{-1}^{1} f (y) g (y) \, {\mathrm {d}}y\). The explicit expression of the matrices \(A_{i},i=1,\dots ,5\) can be found in [10].
Appendix D: Practical aspects for the calculation of the transition number
The practical calculation of the \(P_0\)-term in (34) and the \(P_2\)-term in (35), boils down to the efficient calculation of the inner and trilinear products involved therein. In that respect, we provide here explicit expressions of the latter. They are given by
and
In practice, the integrals can be evaluated by any commonly used quadrature rules in which the values of the integrand are evaluated at quadrature points. In our calculations, we use
where \(y_{n}\) and \(\omega _{n}\) are Legendre–Gauss–Lobatto quadrature points and weights, respectively.
Appendix E: Model parameters
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Chekroun, M.D., Dijkstra, H., Şengül, T. et al. Transitions of zonal flows in a two-layer quasi-geostrophic ocean model. Nonlinear Dyn 109, 1887–1904 (2022). https://doi.org/10.1007/s11071-022-07529-w
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DOI: https://doi.org/10.1007/s11071-022-07529-w