This work is concerned with the inverse problem for ocean acoustics modeled by a multilayered waveguide with a finite depth. We provide explicit formulae to locate the layers, including the seabed, and reconstruct the speed of sound and the densities in each layer from measurements collected on the surface of the waveguide. We proceed in two steps. First, we use Gaussian type excitations on the upper surface of the waveguide and then from the corresponding scattered fields, collected on the same surface, we recover the boundary spectral data of the related 1D spectral problem. Second, from these spectral data, we reconstruct the values of the normal derivatives of the singular solutions, of the original waveguide problem, on that upper surf...
In shallow waters, the fluctuations of the water surface greatly affects the performances of underwa...
Abstract- The propagation of acoustic signals in a waveguide can be efficiently modelled by a parabo...
Time-harmonic acoustic waves in an ocean of finite height are modeled by the Helmholtz equation insi...
This work is concerned with the inverse problem for ocean acoustics modeled by a multilayered wavegu...
The methodology and software developed to reconstruct a vertical sound speed profile as a part of s...
For a source and receiver on the axis of a deep sound channel we solve the two point boundary value ...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 2002.Includes bi...
International audienceThe cross sectional contour of a sound-soft closed cylindrical obstacle placed...
One of main features of shallow water propapagation is the fact that, to great ranges, the acoustic ...
The long-term goal of this research is to increase our understanding of shallow water acoustic propa...
International audienceThe nonlinear retrieval of the cross-sectional contour of a sound-soft or soun...
AbstractA method is derived for computing the acoustic field in a cylindrically symmetric ocean with...
Acoustic wave fields in an ocean waveguide with a sediment layer having continuously varying density...
For this project we constructed a program for calculating the reflection and transmission coefficien...
13p.International audienceThis study demonstrates experimentally at the laboratory scale the detecti...
In shallow waters, the fluctuations of the water surface greatly affects the performances of underwa...
Abstract- The propagation of acoustic signals in a waveguide can be efficiently modelled by a parabo...
Time-harmonic acoustic waves in an ocean of finite height are modeled by the Helmholtz equation insi...
This work is concerned with the inverse problem for ocean acoustics modeled by a multilayered wavegu...
The methodology and software developed to reconstruct a vertical sound speed profile as a part of s...
For a source and receiver on the axis of a deep sound channel we solve the two point boundary value ...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 2002.Includes bi...
International audienceThe cross sectional contour of a sound-soft closed cylindrical obstacle placed...
One of main features of shallow water propapagation is the fact that, to great ranges, the acoustic ...
The long-term goal of this research is to increase our understanding of shallow water acoustic propa...
International audienceThe nonlinear retrieval of the cross-sectional contour of a sound-soft or soun...
AbstractA method is derived for computing the acoustic field in a cylindrically symmetric ocean with...
Acoustic wave fields in an ocean waveguide with a sediment layer having continuously varying density...
For this project we constructed a program for calculating the reflection and transmission coefficien...
13p.International audienceThis study demonstrates experimentally at the laboratory scale the detecti...
In shallow waters, the fluctuations of the water surface greatly affects the performances of underwa...
Abstract- The propagation of acoustic signals in a waveguide can be efficiently modelled by a parabo...
Time-harmonic acoustic waves in an ocean of finite height are modeled by the Helmholtz equation insi...