Stability of solitary waves on deep water with constant vorticity
- 1Institute of Applied Physics RAS, Nonlinear geophysical processes department, Nizhny Novgorod, Russian Federation (dosaev@appl.sci-nnov.ru)
- 2Nizhny Novgorod Planetarium n.a. G. M. Grechko, Nizhny Novgorod, Russian Federation (java-jsp@yandex.ru)
- 3Institute of Applied Physics RAS, Nonlinear geophysical processes department, Nizhny Novgorod, Russian Federation (yuliya@appl.sci-nnov.ru)
Waves on deep water with constant vorticity propagating in the direction of the shear are known to be weakly dispersive in the long wave limit. Weakly-nonlinear evolution of such waves can be described by the Benjamin-Ono equation, which is integrable and has stable soliton solutions. In the present study we investigate behaviour of finite-amplitude counterparts of Benjamin-Ono solitons by modelling their dynamics within exact equations of motion (Euler equations). Due to the solitons having a near-Lorentzian shape with slowly decaying tails, we need to approach them by examining periodic waves, whose crests, indeed, become more and more localised as the period increases. We perform a parameter space study and analyse how stability of very long waves depends on their amplitude and period. We show that large-amplitude solitary waves are unstable.
This research was supported by RFBR (grant No. 16-05-00839) and by the President of Russian Federation (grant No. MK-2041.2017.5). Numerical experiments were supported by RSF grant No. 14-17-00667, data processing was supported by RSF grant No. 15-17-20009.
How to cite: Dosaev, A., Shishina, M., and Troitskaya, Y.: Stability of solitary waves on deep water with constant vorticity, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-10197, https://doi.org/10.5194/egusphere-egu21-10197, 2021.