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Study tsunamis through approximate solution of damped geophysical Korteweg-de Vries equation

  • Received: 04 February 2024 Revised: 06 March 2024 Accepted: 13 March 2024 Published: 19 March 2024
  • MSC : 34K25, 34C27, 34D20, 92D25

  • The article studied tsunami waves with consideration of important wave properties such as velocity, width, and collision through finding an approximate solution to the damped geophysical Korteweg-de Vries (dGKdV). The addition of the damping term in the GKdV is a result of studying the nonlinear waves in bounded nonplanar geometry. The properties of the wave in bounded nonplanar geometry are different than the unbounded planar geometry, as many experiments approved. Thus, this work reported for the first time the analytical solution for the dGKdV equation using the Ansatz method. The used method assumed a suitable hypothesis and the initial condition of the GKdV. The GKdV is an integrable equation and the solution can be found by several known methods either analytically or numerically. On the other hand, the dGKdV is a nonintegrable equation and does not have an initial exact solution, and this is the challenge. In this work, the novel Ansatz method proved its ability to reach the approximate solution of dGKdV and presented the effect of the damping term as well as the Coriolis effect term in the amplitude of the wave. The advantage of the Ansatz method was that the obtained solution was in a general solution form depending on the exact solution of GKdV. This means the variety of nonlinear wave structures like solitons, lumps, or cnoidal can be easily investigated by the obtained solution. We realized that the amplitude of a tsunami wave decreases if the Coriolis term or damping term increases, while it increases if wave speed increases.

    Citation: Noufe H. Aljahdaly. Study tsunamis through approximate solution of damped geophysical Korteweg-de Vries equation[J]. AIMS Mathematics, 2024, 9(5): 10926-10934. doi: 10.3934/math.2024534

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  • The article studied tsunami waves with consideration of important wave properties such as velocity, width, and collision through finding an approximate solution to the damped geophysical Korteweg-de Vries (dGKdV). The addition of the damping term in the GKdV is a result of studying the nonlinear waves in bounded nonplanar geometry. The properties of the wave in bounded nonplanar geometry are different than the unbounded planar geometry, as many experiments approved. Thus, this work reported for the first time the analytical solution for the dGKdV equation using the Ansatz method. The used method assumed a suitable hypothesis and the initial condition of the GKdV. The GKdV is an integrable equation and the solution can be found by several known methods either analytically or numerically. On the other hand, the dGKdV is a nonintegrable equation and does not have an initial exact solution, and this is the challenge. In this work, the novel Ansatz method proved its ability to reach the approximate solution of dGKdV and presented the effect of the damping term as well as the Coriolis effect term in the amplitude of the wave. The advantage of the Ansatz method was that the obtained solution was in a general solution form depending on the exact solution of GKdV. This means the variety of nonlinear wave structures like solitons, lumps, or cnoidal can be easily investigated by the obtained solution. We realized that the amplitude of a tsunami wave decreases if the Coriolis term or damping term increases, while it increases if wave speed increases.



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    [1] D. Dutykh, Mathematical modelling of tsunami waves, École normale supérieure de Cachan-ENS Cachan, 2007.
    [2] E. L. Geist, V. V. Titov, C. E. Synolakis, Tsunami: Wave of change, Sci. Am., 294 (2006), 56–63. https://doi.org/10.1038/scientificamerican0106-56 doi: 10.1038/scientificamerican0106-56
    [3] N. Yaacob, N. M. Sarif, Z. A. Aziz, Modelling of tsunami waves, Malay. J. Indust. Appl. Math., 2008,211–230.
    [4] N. Anjum, Q. T. Ain, X. X. Li, Two-scale mathematical model for tsunami wave, GEM-Int. J. Geomathema., 12 (2021), 10. https://doi.org/10.1007/s13137-021-00177-z doi: 10.1007/s13137-021-00177-z
    [5] I. Didenkulova, E. Pelinovsky, T. Soomere, N. Zahibo, Runup of nonlinear asymmetric waves on a plane beach, Tsunami Nonlinear Wave., 2007,175–190. https://doi.org/10.1007/978-3-540-71256-5_8 doi: 10.1007/978-3-540-71256-5_8
    [6] D. Arcas, H. Segur, Seismically generated tsunamis, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 370 (2012), 1505–1542. https://doi.org/10.1098/rsta.2011.0457
    [7] F. Dias, D. Dutykh, L. O'Brien, E. Renzi, T. Stefanakis, On the modelling of tsunami generation and tsunami inundation, Proc. IUTAM, 10 (2014), 338–355. https://doi.org/10.1016/j.piutam.2014.01.029 doi: 10.1016/j.piutam.2014.01.029
    [8] R. Grimshaw, J. Hunt, K. Chow, Changing forms and sudden smooth transitions of tsunami waves, J. Ocean Eng. Mar. Ener., 1 (2015), 145–156. https://doi.org/10.1007/s40722-014-0011-1 doi: 10.1007/s40722-014-0011-1
    [9] N. Kobayashi, A. R. Lawrence, Cross-shore sediment transport under breaking solitary waves, J. Geophys. Res.-Oceans, 109 (2004). https://doi.org/10.1029/2003JC002084 doi: 10.1029/2003JC002084
    [10] T. Rossetto, W. Allsop, I. Charvet, D. I. Robinson, Physical modelling of tsunami using a new pneumatic wave generator, Coast. Eng., 58 (2011), 517–527. https://doi.org/10.1016/j.coastaleng.2011.01.012 doi: 10.1016/j.coastaleng.2011.01.012
    [11] I. Charvet, I. Eames, T. Rossetto, New tsunami runup relationships based on long wave experiments, Ocean Model., 69 (2013), 79–92. https://doi.org/10.1016/j.ocemod.2013.05.009 doi: 10.1016/j.ocemod.2013.05.009
    [12] A. M. Wazwaz, Solitary waves theory, In: Partial Differential Equations and Solitary Waves Theory, Springer, Berlin, Heidelberg, 2009,479–502. https://doi.org/10.1007/978-3-642-00251-9_12
    [13] N. H. Aljahdaly, R. Shah, R. P. Agarwal, T. Botmart, The analysis of the fractional-order system of third-order KdV equation within different operators, Alex. Eng. J., 61 (2022), 11825–11834. https://doi.org/10.1016/j.aej.2022.05.032 doi: 10.1016/j.aej.2022.05.032
    [14] N. H. Aljahdaly, A. Akgül, R. Shah, I. Mahariq, J. Kafle, A comparative analysis of the fractional-order coupled Lorteweg-de Vries equations with the Mittag-Leffler law, J. Math., 2022 (2022). https://doi.org/10.1155/2022/8876149 doi: 10.1155/2022/8876149
    [15] A. Jha, M. Tyagi, H. Anand, A. Saha, Bifurcation analysis of tsunami waves for the modified geophysical Korteweg-de Vries equation, In: Proceedings of the Sixth International Conference on Mathematics and Computing, Springer, Singapore, 2021, 65–73. https://doi.org/10.1007/978-981-15-8061-1_6
    [16] R. C. McOwen, Partial differential equations: Methods and applications, 2004.
    [17] A. M. Wazwaz, A new integrable nonlocal modified kdv equation: Abundant solutions with distinct physical structures, J. Ocean Eng. Sci., 2 (2017), 1–4. https://doi.org/10.1016/j.joes.2016.11.001 doi: 10.1016/j.joes.2016.11.001
    [18] S. Rizvi, A. R. Seadawy, F. Ashraf, M. Younis, H. Iqbal, D. Baleanu, Lump and interaction solutions of a geophysical Korteweg-de Vries equation, Results Phys., 19 (2020), 103661. https://doi.org/10.1016/j.rinp.2020.103661 doi: 10.1016/j.rinp.2020.103661
    [19] E. H. Zahran, A. Bekir, New unexpected behavior to the soliton arising from the geophysical Korteweg-de Vries equation, Mod. Phys. Lett. B, 36 (2022), 2150623. https://doi.org/10.1142/S0217984921506235 doi: 10.1142/S0217984921506235
    [20] M. Sahoo, S. Chakraverty, Semi-analytical approach to study the geophysical Korteweg-de Vries equation with Coriolis parameter, In: 67th Congress of the Indian Society of Theoretical and Applied Mechanics, 2022.
    [21] T. Ak, A. Saha, S. Dhawan, A. H. Kara, Investigation of Coriolis effect on oceanic flows and its bifurcation via geophysical Korteweg-de Vries equation, Numer. Meth. Part. D. E., 36 (2020), 1234–1253. https://doi.org/10.1002/num.22469 doi: 10.1002/num.22469
    [22] P. Karunakar, S. Chakraverty, Effect of Coriolis constant on geophysical Korteweg-de Vries equation, J. Ocean Eng. Sci., 4 (2019), 113–121. https://doi.org/10.1016/j.joes.2019.02.002 doi: 10.1016/j.joes.2019.02.002
    [23] H. Bailung, S. Sharma, A. Boruah, T. Deka, Y. Bailung, Experimental observation of cylindrical dust acoustic soliton in a strongly coupled dusty plasma, In: 2nd Asia-Pacific Conference on Plasma Physics, Kanazawa, Japan, 2018, 12–17.
    [24] N. H. Aljahdaly, S. El-Tantawy, Novel anlytical solution to the damped Kawahara equation and its application for modeling the dissipative nonlinear structures in a fluid medium, J. Ocean Eng. Sci., 7 (2022), 492–497. https://doi.org/10.1016/j.joes.2021.10.001 doi: 10.1016/j.joes.2021.10.001
    [25] M. Alharthi, R. Alharbey, S. El-Tantawy, Novel analytical approximations to the nonplanar Kawahara equation and its plasma applications, Eur. Phys. J. Plus, 137 (2022), 1–10. https://doi.org/10.1140/epjp/s13360-022-03355-6 doi: 10.1140/epjp/s13360-022-03355-6
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