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Elementary properties of non-Linear Rossby-Haurwitz planetary waves revisited in terms of the underlying spherical symmetry

  • Received: 30 October 2018 Accepted: 06 March 2019 Published: 19 March 2019
  • MSC : 76U99, 22E70

  • We revisit Rossby-Haurwitz planetary wave modes of a two-dimensional fluid along the surface of a rotating planet, as elements of irreducible representations of the so(3) Lie algebra. Key questions addressed are, firstly, why it is that the non-linear self-interaction of any Rossby-Haurwitz wave mode is zero, and secondly, why the phase velocity of these wave modes is insensitive to their orientation with respect to the axis of rotation of the planet, while at the same time the very rotation of the planet is a precondition for the existence of the waves. As we show, answers to both questions can be rooted in Lie group and representation theory. In our study the Rossby-Haurwitz modes emerge in a coordinate-free, as well as in a Ricci tensor rank-free manner. We find them with respect to a continuum of spherical coordinate systems, that are arbitrarily oriented with respect to the planet. Furthermore, we show that, in the same sense in which the Lie derivative of Ricci tensor fields is rankfree, the wave equation for Rossby-Haurwitz modes is rank-free. We find that, for each irreducible representation of so(3), there is a corresponding sufficient condition for existence of Rossby-Haurwitz modes as solutions that are separable with respect to space and time. This condition comes in the form of a system of equations of motion for the coordinate systems. Coordinate systems that move along with Rossby-Haurwitz modes emerge as special cases of these. In these coordinate systems the waves appear as stationary spatial fields, so that the motion of the coordinate system coincides with the wave phase propagation. The general solution of the existence condition is a continuum of moving spherical coordinate systems that precess about the axes of the Rossby-Haurwitz modes. Within a single irreducible representation of so(3), the waves are dispersionless.

    Citation: Ramses van der Toorn. Elementary properties of non-Linear Rossby-Haurwitz planetary waves revisited in terms of the underlying spherical symmetry[J]. AIMS Mathematics, 2019, 4(2): 279-298. doi: 10.3934/math.2019.2.279

    Related Papers:

  • We revisit Rossby-Haurwitz planetary wave modes of a two-dimensional fluid along the surface of a rotating planet, as elements of irreducible representations of the so(3) Lie algebra. Key questions addressed are, firstly, why it is that the non-linear self-interaction of any Rossby-Haurwitz wave mode is zero, and secondly, why the phase velocity of these wave modes is insensitive to their orientation with respect to the axis of rotation of the planet, while at the same time the very rotation of the planet is a precondition for the existence of the waves. As we show, answers to both questions can be rooted in Lie group and representation theory. In our study the Rossby-Haurwitz modes emerge in a coordinate-free, as well as in a Ricci tensor rank-free manner. We find them with respect to a continuum of spherical coordinate systems, that are arbitrarily oriented with respect to the planet. Furthermore, we show that, in the same sense in which the Lie derivative of Ricci tensor fields is rankfree, the wave equation for Rossby-Haurwitz modes is rank-free. We find that, for each irreducible representation of so(3), there is a corresponding sufficient condition for existence of Rossby-Haurwitz modes as solutions that are separable with respect to space and time. This condition comes in the form of a system of equations of motion for the coordinate systems. Coordinate systems that move along with Rossby-Haurwitz modes emerge as special cases of these. In these coordinate systems the waves appear as stationary spatial fields, so that the motion of the coordinate system coincides with the wave phase propagation. The general solution of the existence condition is a continuum of moving spherical coordinate systems that precess about the axes of the Rossby-Haurwitz modes. Within a single irreducible representation of so(3), the waves are dispersionless.


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    [1] D. Brink and G. Satchler, Angular Momentum, Oxford Library of the Physical Sciences, Oxford University Press, Oxford, 1962.
    [2] E. Butkov, Mathematical Physics, Addison-Wesley Publishing Company, 1968.
    [3] S. Chandrasekhar, Ellipsoidal Figures of Equilibrium, Yale University Press, 1969.
    [4] J. Cornwell, Group Theory in Physics An Introduction, Academic Press, San Diego, 1997.
    [5] R. Craig, A solution for the nonlinear vorticity equation for atmospheric motion, J. Meteor., 2 (1945), 175-178. doi: 10.1175/1520-0469(1945)002<0175:ASOTNV>2.0.CO;2
    [6] P. J. Dellar, Variations on a beta-plane: derivation of non-traditional beta-plane equations from Hamilton's principle on a sphere, J. Fluid Mech., 674 (2011), 174-195. doi: 10.1017/S0022112010006464
    [7] B. A. Dubrovin, A. T. Fomenko and S. P. Novikov, Modern Geometry, Methods and Applications, Part 1, Graduate Texts in Mathematics, Spinger-Verlag, New York, 1992.
    [8] H. Flanders, Differential Form with Applications to the Physical Sciences, Mathematics in Science and Engineering, Academic Press, New York, 1963.
    [9] B. Haurwitz, The motion of atmospheric disturbances on a spherical earth, Journal of Marine Research, 3 (1940).
    [10] M. C. Hendershott, Long waves and ocean tides, in Evolution of Physical Oceanography (eds. B. A. Warren and C. Wunsch), MIT Press, Cambridge, Massac, 1981, 292-341.
    [11] J. R. Holton, An Introduction to Dynamic Meteorology, vol. 48 of International Geophysics Series, 3rd edition, Academic Press, 1992.
    [12] S. S. Hough, On the application of harmonic analysis to the dynamical theory of the tides - Part I. On Laplace's "Oscillations of the first species", and on the dynamics of ocean currents, Phil. Trans. R. Soc. London. Ser. A., 189 (1897), 201-257. doi: 10.1098/rsta.1897.0009
    [13] S. S. Hough, On the application of harmonic analysis to the dynamical theory of the tides - Part II. On the general integration of Laplace's dynamical equations, Phil. Trans. R. Soc. London. Ser. A., 191 (1898), 139-185. doi: 10.1098/rsta.1898.0005
    [14] M. S. Longuet-Higgins, Planetary waves on a rotating sphere, Proc. Roy. Soc. London, A, 279 (1964), 446-473. doi: 10.1098/rspa.1964.0116
    [15] P. Lynch, On resonant Rossby-Haurwitz triads, Tellus, 61A (2009), 438-445.
    [16] J. Pedlosky, Geophysical Fluid Dynamics, Spinger-Verlag, New York, 1987.
    [17] G. W. Platzman, The spectral form of the vorticity equation, Journal of Meteorology, 17 (1960), 635-644. doi: 10.1175/1520-0469(1960)017<0635:TSFOTV>2.0.CO;2
    [18] G. W. Platzman, The analytical dynamics of the spectral vorticity equation, J. Atmos. Sci., 19 (1962), 313-327. doi: 10.1175/1520-0469(1962)019<0313:TADOTS>2.0.CO;2
    [19] M. Rose, Elementary Theory of Angular Momentum, John Wiley & Sons, New York, 1957.
    [20] C. Rossby, Relations between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semi-permanent centers of action, Journal of Marine Research, 2 (1939), 38-55. doi: 10.1357/002224039806649023
    [21] I. S. Sokolnikoff, Tensor Analysis; Theory and Applications to Geometry and Mechanics of Continua, 2nd edition, John Wiley and Sons, Inc., 1964,
    [22] P. D. Thompson, A generalized class of exact time-dependent solutions of the vorticity equation for nondivergent barotropic flow, Monthly Weather Review, 110 (1982), 1321-1324. doi: 10.1175/1520-0493(1982)110<1321:AGCOET>2.0.CO;2
    [23] R. van der Toorn and J. T. F. Zimmerman, On the spherical approximation of the geopotential in geophysical fluid dynamics and the use of a spherical coordinate system, Geophys. Astrophys. Fluid Dyn., 102 (2008), 349-371. doi: 10.1080/03091920801900674
    [24] R. Van der Toorn and J. T. F. Zimmerman, Angular momentum dynamics and the intrinsic drift of monopolar vortices on a rotating sphere, J. Math. Phys., 51 (2010), 83102.
    [25] W. Verkley, The construction of barotropic modons on a sphere, J. Atmos. Sci., 40 (1984), 2492-2504.
    [26] A. White, B. Hoskins, I. Roulstone, et al. Consistent approximate models of the global atmosphere: Shallow, deep hydrostatic and non-hydrostatic, Quar. J. Roy. Met. Soc., 131 (2005), 2081-2107. doi: 10.1256/qj.04.49
    [27] E. P. Wigner, Group Theory, Academic Press, New York, 1959.
    [28] Wolfram Research, Inc., Mathematica, Version 11.3, Champaign, IL, 2018.
    [29] R. Zhang, L. Yang, Q. Liu, et al. Dynamics of nonlinear Rossby waves in zonally flow with spatial-temporal varying topography, Appl. Math. Comput., 346 (2019), 666-679.
    [30] R. Zhang, L. Yang, J. Song, et al. (2+1) dimensional nonlinear Rossby solitary waves under the effects of generalized beta and slowly varying topography, Nonlinear Dynamics, 90 (2017), 815-822. doi: 10.1007/s11071-017-3694-8
    [31] R. Zhang, L. Yang, J. Song, et al. (2+1) dimensional Rossby waves with complete coriolis force and its solution by homotopy perturbation method, Comput. Math. Appl., 73 (2017), 1996-2003. doi: 10.1016/j.camwa.2017.02.036
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