A backscattering model based on corrector theory of homogenization for the random Helmholtz equation

TL;DR

This paper develops a homogenization corrector model for wave backscattering in random media like sea ice, accounting for non-normal incidence and deriving a transport model for high-frequency wavefields.

Contribution

It introduces a novel backscattering model based on corrector theory for the random Helmholtz equation, addressing non-normal incidence in layered random media.

Findings

Derived an explicit expression for the homogenization corrector.

Established a transport model for quadratic wavefield quantities.

Analyzed the impact of non-normal incidence on backscattered signals.

Abstract

This work concerns the analysis of wave propagation in random media. Our medium of interest is sea ice, which is a composite of a pure ice background and randomly located inclusions of brine and air. From a pulse emitted by a source above the sea ice layer, the main objective of this work is to derive a model for the backscattered signal measured at the source/detector location. The problem is difficult in that, in the practical configuration we consider, the wave impinges on the layer with a non-normal incidence. Since the sea ice is seen by the pulse as an effective (homogenized) medium, the energy is specularly reflected and the backscattered signal vanishes in a first order approximation. What is measured at the detector consists therefore of corrections to leading order terms, and we focus in this work on the homogenization corrector. We describe the propagation by a random Helmholtz equation, and derive an expression of the corrector in this layered framework. We moreover obtain a transport model for quadratic quantities in the random wavefield in a high frequency limit.