Geometric decorrelation in acoustic tools for surveying the seafloor

The purpose of the present work is to establish decorrelation estimates for the eigenvalues of the discrete Anderson model localized near two distinct energies inside the

We now consider the response of the climatic oscillator described by eqs. Our purpose is to show that the forcing provides the synchroni- zing element that was

Considering the scarcity of studies regarding modern tsunami impacts on shallow-water benthic marine environments 5–7 , offshore imprints related to tsunami run- up and backwash

We proposed a methodology to analyze the precision on the vegetation height estimation using the PolInSAR sys- tem in the DB configuration with an RVoG model, where the

The partially/totally asym- metric simple exclusion process (P/TASEP), last passage percolation (LPP) with exponential or geometric weights, the corner growth model, and

The application of the MFS for the acoustic wave scat- tering by porous scatterers has been presented. The wave equations for the fluid phase and solid phase displace- ments can

A geodesic triangle on Riemannian manifold is a triangle all of whose ver- tices are geodesics.. On a sphere, for example, the curvature is always 1 which means that the sum of

3.5] which remains valid although parts of its proof require some corrections that we now explain.. Proof of Proposition 3.5