Three-dimensional time-domain scattering of waves in the marginal ice zone

Abstract

Three-dimensional scattering of ocean surface waves in the marginal ice zone (MIZ) is determined in the time domain. The solution is found using spectral analysis of the linear operator for the Boltzmann equation. The method to calculate the scattering kernel that arises in the Boltzmann model from the single-floe solution is also presented along with new identities for the far-field scattering, which can be used to validate the single-floe solution. The spectrum of the operator is computed, and it is shown to have a universal structure under a special non-dimensionalization. This universal structure implies that under a scaling wave scattering in the MIZ has similar properties for a large range of ice types and wave periods. A scattering theory solution using fast Fourier transforms is given to find the solution for directional incident wave packets. A numerical solution method is also given using the split-step method and this is used to validate the spectral solution. Numerical calculations of the evolution of a typical wave field are presented.

Document Details

Document Type
Pub Defense Publication
Publication Date
Aug 20, 2018
Source ID
10.1098/rsta.2017.0334

Entities

People

  • L. G. Bennetts
  • Michael Meylan

Organizations

  • Engineering and Physical Sciences Research Council
  • Office of Naval Research
  • Simons Foundation
  • University of Adelaide
  • University of Newcastle

Tags

Fields of Study

  • Physics

Readers

  • Electromagnetic Wave Scattering and Antenna Radiation Engineering
  • Polar and Arctic Studies
  • Wave Propagation and Nonlinear Chaotic Dynamics.