Geoacoustic inversion for the seabed transition layer using a Bernstein polynomial model

Keyphrases

• Transition Layer 100%
• Geoacoustic Inversion 100%
• Geoacoustics 100%
• Parametrization 66%
• Depth-dependent 66%
• Enhanced Resolution 33%
• Small Perturbation 33%
• Parameter Space 33%
• Centimeter-scale 33%
• Density Profile 33%
• Inversion Method 33%
• Low Uncertainty 33%
• Number of Parameters 33%
• Efficient Exploration 33%
• Sound Speed Profile 33%
• Malta Plateau 33%
• Geoacoustic Parameters 33%
• Polynomial Representation 33%
• Local Perturbation 33%
• Sediment-water Interface 33%
• Nonlinear Inversion 33%
• Bernstein 33%
• Resolution Improvement 33%

Engineering

• Parametrization 100%
• Bernstein Polynomial 100%
• Polynomial Model 100%
• Basis Function 50%
• Parameter Space 50%
• Centimeter 50%
• Sound Speed 50%
• Inversion Method 50%

Earth and Planetary Sciences

• Markov Chain 100%
• Malta 100%
• Sediment-Water Interface 100%