Abstract
Taking into account the coupling of the ocean with the atmosphere is essential to properly describe vortex dynamics in the ocean. The forcing of a circular eddy with the relative wind stress curl leads to an Ekman pumping with a nonzero area integral. This in turn creates a source or a sink in the eddy. We revisit the two point vortex-source interaction, now coupled with an unsteady wind, leading to a time-varying circulation and source strength. Firstly, we recover the various fixed points of the two vortex-source system, and we calculate their stability. Then we show the effect of a weak amplitude, subharmonic, or harmonic time variation of the wind, leading to a similar variation of the circulation and the source strength of the vortex sources. We use a multiple time scale expansion of the variables to calculate the long time variation of these vortex trajectories around neutral fixed points. We study the amplitude equation and obtain its solution. We compute numerically the unstable evolution of the vortex sources when the source and circulation have a finite periodic variation. We also assess the influence of this time variation on the dispersion of a passive tracer near these vortex sources.
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References
Aref, H., Integrable, Chaotic, and Turbulent Vortex Motion in Two-Dimensional Flows, Annu. Rev. Fluid Mech., 1983, vol. 15, pp. 345–389.
Aref, H. and Pomphrey, N., Integrable and Chaotic Motions of Four Vortices, Phys. Lett. A, 1980, vol. 78, no. 4, pp. 297–300.
Bizyaev, I. A., Borisov, A. V., and Mamaev, I. S., The Dynamics of Vortex Sources in a Deformation Flow, Regul. Chaotic Dyn., 2016, vol. 21, no. 3, pp. 367–376.
Borisov, A. V. and Mamaev, I. S., On the Problem of Motion Vortex Sources on a Plane, Regul. Chaotic Dyn., 2006, vol. 11, no. 4, pp. 455–466.
Carton, X. J., Hydrodynamical Modelling of Oceanic Vortices, Surv. Geophys., 2001, vol. 22, no. 3, pp. 179–263.
Carton, X., Oceanic Vortices, in Fronts, Waves and Vortices in Geophysical Flows, , J. B. Flor (Ed.), Lect. Notes Phys., Berlin: Springer, 2010, pp. 61–108.
Carton, X., Morvan, M., Reinaud, J. N., Sokolovskiy, M. A., L’Hégaret, P., and Vic, C., Vortex Merger near a Topographic Slope in a Homogeneous Rotating Fluid, Regul. Chaotic Dyn., 2017, vol. 22, no. 5, pp. 455–478.
Chelton, D. B., Schlax, M. G., Samelson, R. M., and de Szoeke, R. A., Global Observations of Large Oceanic Eddies, Geophys. Res. Lett., 2007, vol. 34, no. 15, L15606, 5 pp.
Dritschel, D. G., A General Theory for Two-Dimensional Vortex Interactions, J. Fluid Mech., 1995, vol. 293, pp. 269–303.
Dritschel, D. G., Vortex Merger in Rotating Stratified Flows, J. Fluid Mech., 2002, vol. 455, pp. 83–101.
Koshel, K. V. and Ryzhov, E. A., Parametric Resonance with a Point-Vortex Pair in a Nonstationary Deformation Flow, Phys. Lett. A, 2012, vol. 376, no. 5, pp. 744–747.
Koshel, K. V., Reinaud, J. N., Riccardi, G., and Ryzhov, E. A., Entrapping of a Vortex Pair Interacting with a Fixed Point Vortex Revisited: 1. Point Vortices, Phys. Fluids, 2018, vol. 30, no. 9, 096603, 22 pp.
Koshel, K. V., Ryzhov, E. A., and Carton, X. J., Vortex Interactions Subjected to Deformation Flows: A Review, Fluids, 2019, vol. 4, no. 1, Art. 14, 48 pp.
Newton, P. K., Point Vortex Dynamics in the Post-Aref Era, Fluid Dynam. Res., 2014, vol. 46, no. 3, 031401, 11 pp.
Perrot, X. and Carton, X., Point-Vortex Interaction in an Oscillatory Deformation Field: Hamiltonian Dynamics, Harmonic Resonance and Transition to Chaos, Discrete Contin. Dyn. Syst. Ser. B, 2009, vol. 11, no. 4, pp. 971–995.
Perrot, X. and Carton, X., 2D Vortex Interaction in Anon-Uniform Flow, Theor. Comput. Fluid Dyn., 2010, vol. 24, no. 1, pp. 95–100.
Płotka, H. and Dritschel, D. G., Quasi-Geostrophic Shallow-Water Doubly-Connected Vortex Equilibria and Their Stability, J. Fluid Mech., 2013, vol. 723, pp. 40–68.
Reinaud, J. N. and Dritschel, D. G., The Merger of Vertically Offset Quasi-Geostrophic Vortices, J. Fluid Mech., 2002, vol. 469, pp. 287–315.
Reinaud, J. N. and Dritschel, D. G., The Critical Merger Distance between Two Co-Rotating Quasi-Geostrophic Vortices, J. Fluid Mech., 2005, vol. 522, pp. 357–381.
Reinaud, J. N. and Carton, X., The Stability and the Nonlinear Evolution of Quasi-Geostrophic Hetons, J. Fluid Mech., 2009, vol. 636, pp. 109–135.
Renault, L., McWilliams, J. C., and Gula, J., Dampening of Submesoscale Currents by Air-Sea Stress Coupling in the Californian Upwelling System, Sci. Rep., 2018, vol. 8, 13388, 8 pp.
Renault, L., Marchesiello, P., Masson, S., and McWilliams, J. C., Remarkable Control of Western Boundary Currents by Eddy Killing, a Mechanical Air-Sea Coupling Process, Geophys. Res. Lett., 2019, vol. 46, no. 5, pp. 2743–2751.
Sokolovskiy, M. A., Koshel, K. V., and Carton, X., Baroclinic Multipole Evolution in Shear and Strain, Geophys. Astrophys. Fluid Dyn., 2011, vol. 105, nos. 4–5, pp. 506–535.
Sokolovskiy, M. A. and Verron, J., Finite-Core Hetons: Stability and Interactions, J. Fluid Mech., 2000, vol. 423, pp. 127–154.
Sokolovskiy, M. A., Carton, X. J., and Filyushkin, B. N., Mathematical Modeling of Vortex Interaction Using a Three-Layer Quasigeostrophic Model: Part 1. Point-Vortex Approach, Mathematics, 2020, vol. 8, no. 8, Art. 1228, 13 pp.
ACKNOWLEDGMENTS
The first author thanks Ecole Normale Superieure de Rennes (Maths Department) for a Ph.D. grant allowing the completion of this work.
The authors thanks Dr Jean N. Reinaud for proofreading and the English writing of this paper.
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MSC2010
34D20
APPENDIX A. EQUILIBRIUM POINTS AND STABILITY
This section is a reminder of the fixed points of the problem; it was addressed slightly differently in [4] and in [3]. Recall the various cases for equilibria here with our notations and in our specific cases. This is necessary to further study the vortex source evolution with unsteady circulation or source strength.
Recall that we have the condition \(\Gamma_{0}\Omega<0\) and the formulas
6.1. For \(\Omega^{2}=A^{2}\):
Equilibrium. Starting from Eq. (A.3) with \(\Omega^{2}=A^{2}\) and \(\Gamma_{0}\Omega<0\), we have \(r_{0}^{2}=-\frac{S_{0}^{2}+\Gamma_{0}^{2}}{8\pi\Gamma_{0}\Omega}>0\) and thanks to Eq. (A.1), we have
Stability. Is the equilibrium (A.4) stable? From the characteristic polynomial (3.7) of the differential matrix \(\chi(X)=X^{2}-\frac{S_{0}^{2}+\Gamma_{0}^{2}+4\pi r_{0}^{2}\Gamma_{0}\Omega}{4\pi^{2}r_{0}^{4}}\), we need to determine the sign of \(\Delta_{0}\):
6.2. For \(\Omega^{2}\neq A^{2}\):
From the polynomial equation (A.3) in \(r_{0}^{2}\):
we compute the discriminant
and look at the sign of
We want \(\Delta^{\prime}\) to be positive because we want real (positive) solutions to Eq. (A.6). This brings three situations (we have already studied the situation \(\Omega^{2}=A^{2}\)):
-
If \(A^{2}>\Omega^{2}\), then \(\Delta^{\prime}>0\) clearly from Eq. (A.9).
-
If \(\Omega^{2}>A^{2}\), then \(\Delta^{\prime}>0\iff\Omega^{2}<A^{2}\left(1+\frac{\Gamma_{0}^{2}}{S_{0}^{2}}\right)\).
-
If \(\Omega^{2}=A^{2}\left(1+\frac{\Gamma_{0}^{2}}{S_{0}^{2}}\right)\), then \(\Delta^{\prime}=0\).
Because \(A^{2}>\Omega^{2}\), we have \(\Delta^{\prime}>0\) without any more condition, and we have two solutions to the polynomial equation (A.6):
Equilibrium for \(X_{+}\). We have the following equilibrium point (with \(\theta_{0}\) computed from Eq. (A.1)):
Stability for \(X_{+}\). How is the equilibrium (A.11) stable? We need to know the sign of \(\Delta_{0}\).
Proposition 1
Under all the conditions of this subsection, we have
Proof
Remember that we work under the assumption \(A^{2}>\Omega^{2}\) and \(\Gamma_{0}\Omega<0\). Then put \(r_{0}^{2}\) in \(\Delta_{0}\) and
We also have two roots of the polynomial (A.6):
Equilibrium and stability for \(X_{+}\). We have the following equilibrium point (with \(\theta_{0}\) computed from Eq. (A.1)):
Proposition 2
Whatever the set of parameters we choose, if they satisfy the assumptions we made: \(A^{2}<\Omega^{2}<A^{2}\left(1+\frac{\Gamma_{0}^{2}}{S_{0}^{2}}\right)\) and \(\Gamma_{0}\Omega<0\) , then we have
Proof
Consider \(\Delta_{0}\) for the value \(r_{0}\) we have in Eq. (A.13):
Equilibrium and stability for \(X_{-}\). We have the following equilibrium point (with \(\theta_{0}\) computed from Eq. (A.1)):
Proposition 3
For the equilibrium (A.15) , \(\Delta_{0}\) is nonnegative for every set of parameters such that \(A^{2}<\Omega^{2}<A^{2}\left(1+\frac{\Gamma_{0}^{2}}{S_{0}^{2}}\right)\) and \(\Gamma_{0}\Omega<0\) . So the equilibrium (A.15) is a saddle equilibrium point.
Proof
Look at the expression of \(\Delta_{0}\):
In this section, we have \(\Delta^{\prime}=0\). Then there is only one solution to Eq. (A.6):
APPENDIX B. MULTIPLE TIME SCALE DEVELOPMENT
The multiple time scale method is here expanded for the subharmonic case. The harmonic case is similar.
6.1. Order \(\varepsilon^{1}\)
We have the following system at order \(\varepsilon^{1}\), computed from Eqs. (4.5) and (4.8):
6.2. Order \(\varepsilon^{2}\)
With Eqs. (4.6) and (4.9) and because \(\partial_{t_{1}}r_{1}=\partial_{t_{1}}\left(r_{0}\theta_{1}\right)=0\), we have the following system in \((r_{2},r_{0}\theta_{2})\):
where
The system (B.4) gives:
-
For \(r_{2}\):
$$\displaystyle\partial_{t_{0}}^{2}r_{2}=-a\left(-ar_{2}-b\left(r_{0}\theta_{2}\right)+f_{2}\right)-b\left(-cr_{2}+a\left(r_{0}\theta_{2}\right)+g_{2}\right)+\partial_{t_{0}}f_{2}$$$$\displaystyle=\left(a^{2}+bc\right)r_{2}+h_{2}(t_{0},t_{1},t_{2},t_{3}).$$(B.6) -
For \(r_{0}\theta_{2}\):
$$\displaystyle\partial_{t_{0}}^{2}\left(r_{0}\theta_{2}\right)=-c\left(-ar_{2}-b\left(r_{0}\theta_{2}\right)+f_{2}\right)+a\left(-cr_{2}+a\left(r_{0}\theta_{2}\right)+g_{2}\right)+\partial_{t_{0}}g_{2}$$$$\displaystyle=\left(bc+a^{2}\right)\left(r_{0}\theta_{2}\right)+k_{2}(t_{0},t_{1},t_{2},t_{3}),$$(B.7)
where
-
Development of \(f_{2}\):
$$\displaystyle f_{2}=\frac{a}{r_{0}}\left[3-\frac{2c}{b}\right]|C_{1,1}|^{2}$$$$\displaystyle+\left[\frac{ar_{0}}{4}+\frac{C_{1,1}^{2}}{r_{0}}\left(\frac{3a}{2}+\frac{a\left(a+i\omega_{0}\right)^{2}}{b^{2}}+i\omega_{0}\right)\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}$$$$\displaystyle f_{2}=F_{2,0}|C_{1,1}|^{2}+\left[F_{2,2,1}+F_{2,2,2}C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}.$$(B.9) -
Development of \(g_{2}\):
$$\displaystyle g_{2}=\frac{c}{r_{0}}|C_{1,1}|^{2}+\left[\frac{cr_{0}}{4}+\frac{C_{1,1}^{2}}{r_{0}}\left(\frac{3c}{2}+\frac{\left(a+i\omega_{0}\right)^{2}}{b}\right)\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}$$$$\displaystyle g_{2}=G_{2,0}|C_{1,1}|^{2}+\left[G_{2,2,1}+G_{2,2,2}C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}.$$(B.10) -
Development of \(h_{2}\):
$$\displaystyle h_{2}=\left[-aF_{2,0}-bG_{2,0}\right]|C_{1,1}|^{2}+\left[\left(-bG_{2,2,1}+\left(-a+2i\omega_{0}\right)F_{2,2,1}\right)\right.$$$$\displaystyle\left.+\left(-bG_{2,2,2}+\left(-a+2i\omega_{0}\right)F_{2,2,2}\right)C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}$$$$\displaystyle h_{2}=H_{2,0}|C_{1,1}|^{2}+\left[H_{2,2,1}+H_{2,2,2}C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}.$$(B.11) -
Development of \(k_{2}\):
$$\displaystyle k_{2}=\left[-cF_{2,0}+aG_{2,0}\right]|C_{1,1}|^{2}+\left[\left(-cF_{2,2,1}+\left(a+2i\omega_{0}\right)G_{2,2,1}\right)\right.$$$$\displaystyle\left.+\left(-cF_{2,2,2}+\left(a+2i\omega_{0}\right)G_{2,2,2}\right)C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}$$$$\displaystyle k_{2}=K_{2,0}|C_{1,1}|^{2}+\left[K_{2,2,1}+K_{2,2,2}C_{1,1}^{2}\right]\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}.$$(B.12)
Then from Eqs. (B.6) and (B.7) we have
-
The homogeneous solutions:
$$\begin{cases}r_{2}=C_{2,1}\mathrm{e}^{i\omega_{0}t_{0}}+\mathrm{c.c}\\ \left(r_{0}\theta_{2}\right)=D_{2,1}\mathrm{e}^{i\omega_{0}t_{0}}+\mathrm{c.c}\end{cases}$$(B.13) -
The particular solutions for the constant terms:
$$\begin{cases}r_{2}=\frac{H_{2,0}}{\omega_{0}^{2}}|C_{1,1}|^{2}\\ \left(r_{0}\theta_{2}\right)=\frac{K_{2,0}}{\omega_{0}^{2}}|C_{1,1}|^{2}\end{cases}$$(B.14) -
The particular solutions for \(\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}\):
$$\begin{cases}r_{2}=-\frac{H_{2,2,1}+H_{2,2,2}C_{1,1}^{2}}{3\omega_{0}^{2}}\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}\\ \left(r_{0}\theta_{2}\right)=-\frac{K_{2,2,1}+K_{2,2,2}C_{1,1}^{2}}{3\omega_{0}^{2}}\mathrm{e}^{2i\omega_{0}t_{0}}+\mathrm{c.c}.\end{cases}$$(B.15)
So the total solution of Eqs. (B.6) and (B.7) is
6.3. Order \(\varepsilon^{3}\)
With Eqs. (4.7) and (4.10), we have the following system at the order \(\varepsilon^{3}\):
-
For \(r_{3}\):
$$\displaystyle\partial_{t_{0}}^{2}r_{3}=-a\left(-ar_{3}-b\left(r_{0}\theta_{3}\right)+f_{3}\right)-b\left(-cr_{3}+a\left(r_{0}\theta_{3}\right)+g_{3}\right)+\partial_{t_{0}}f_{3}$$$$\displaystyle=\left(a^{2}+bc\right)r_{3}+h_{3}.$$(B.20) -
For \(r_{0}\theta_{3}\):
$$\displaystyle\partial_{t_{0}}^{2}\left(r_{0}\theta_{3}\right)=-c\left(-ar_{3}-b\left(r_{0}\theta_{3}\right)+f_{3}\right)+a\left(-cr_{3}+a\left(r_{0}\theta_{3}\right)+g_{3}\right)+\partial_{t_{0}}g_{3}$$$$\displaystyle=\left(bc+a^{2}\right)\left(r_{0}\theta_{3}\right)+k_{3}.$$(B.21)
We do not develop \(f_{3},\ g_{3},\ h_{3}\) and \(k_{3}\) as we did for the order \(\varepsilon^{2}\). We only introduce the following notations:
Then, if we denote by \(L\) the self-adjoint linear operator \(\partial_{t_{0}}^{2}+\omega_{0}^{2}\), we have \(r_{1}^{\star}Lr_{3}=r_{1}^{\star}h_{3}=r_{1}^{\star}L^{\star}r_{3}=0=\langle r_{1},h_{3}\rangle\). But \(\langle e^{in\omega_{0}t_{0}},e^{ip\omega_{0}t_{0}}\rangle=\delta_{n,p}\) (Kronecker symbol) for \(n,p\in\mathbf{Z}\) and because \(r_{1}=C_{1,1}\mathrm{e}^{i\omega_{0}t_{0}}+\mathrm{c.c}\), we have
Because \(H_{3,1}=(-a+i\omega_{0})F_{3,1}-bG_{3,1}\), we deduce the amplitude equation
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Vic, A., Carton, X. & Gula, J. The Interaction of Two Unsteady Point Vortex Sources in a Deformation Field in 2D Incompressible Flows. Regul. Chaot. Dyn. 26, 618–646 (2021). https://doi.org/10.1134/S1560354721060034
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DOI: https://doi.org/10.1134/S1560354721060034