EGU2020-3204, updated on 12 Jun 2020
https://doi.org/10.5194/egusphere-egu2020-3204
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

A nonlinear Schrödinger equation for gravity waves slowly modulated by linear shear flow

Shaofeng Li, Juan Chen, Anzhou Cao, and Jinbao Song
Shaofeng Li et al.
  • Zhejiang University, Ocean College, China (lishaofeng@zju.edu.cn)

Assume that a fluid is inviscid, incompressible, and irrotational. A nonlinear Schrödinger equation (NLSE) describing the evolution of gravity waves in finite water depth is derived using the multiple scale analysis method. The gravity waves are influenced by a linear shear flow, which is composed of a uniform flow and a shear flow with constant vorticity. The modulational instability (MI) of the NLSE was analyzed in this paper, and the region of MI for gravity waves (the necessary condition for the existence of freak waves) was identified. In this paper, the uniform background flows along or against wave propagation are referred to as down-flow and up-flow, respectively. Uniform up-flow enhances the MI, whereas uniform down-flow reduces it. Positive vorticity enhances the MI, while negative vorticity reduces it. Hence, the influence of positive (negative) vorticity on MI can be balanced out by that of uniform down- (up-)flow. Furthermore, the Peregrine breather (PB) solution of the NLSE is applied to freak waves. Uniform up-flow increases the steepness of free surface elevation, while uniform down-flow decreases it. Positive vorticity increases the steepness of free surface elevation, whereas negative vorticity decreases it.

How to cite: Li, S., Chen, J., Cao, A., and Song, J.: A nonlinear Schrödinger equation for gravity waves slowly modulated by linear shear flow, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3204, https://doi.org/10.5194/egusphere-egu2020-3204, 2020