E. Cherkaev | Searcharxiv

arXiv2024

Bounds on the complex viscoelasticity for surface waves on ice-covered seas

Oceanic wave propagation through Earth's sea ice covers is a critical component of accurate ice and climate modeling. Continuum models of the polar ocean surface layer are characterized rheologically by the effective complex viscoelasticity of the composite of ice floes and sea water. Here we present the first rigorous theory of this parameter, and distill its dependence on mixture geometry into the spectral properties of a self-adjoint operator analogous to the Hamiltonian in quantum physics. Bounds for the complex viscoelasticity are obtained from the sea ice concentration and the contrast between the elastic and viscous properties of the ice and water/slush constituents. We find that several published wave attenuation datasets in both laboratory and field settings fall well within the bounds for specific contrast values of the ice/ocean composite.

physics.geo-ph↗

arXiv2024

Iterative bounds on effective transport for advection diffusion in periodic flow fields

Over three decades ago a Stieltjes integral representation for the effective diffusivity of a tracer in a steady fluid velocity field was developed, involving the spectral measure of a compact self-adjoint operator and the P\'eclet number of the flow. Rigorous bounds on the homogenized diffusivity could then be obtained from knowledge of the moments of the spectral measure. A recent extension to space-time periodic flows involves an unbounded self-adjoint operator. Though Pad\'e approximants provide upper and lower bounds in terms of the moments, the lack of a general method for calculating them has significantly limited the utility of this approach. Here we develop an iterative method that enables an arbitrary number of moments, hence bounds, to be calculated analytically in closed form for spatially and space-time periodic flows. The known behavior of the effective diffusivity for a 2D steady cellular flow is accurately captured by high order upper and lower bounds. The bounds extend to 3D steady and time periodic flow fields away from the advection dominated regime where an open issue remains concerning the divergence of the bounds.

physics.flu-dyn↗