Related Experiment Video
Updated: Jun 12, 2026

Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
Inversion for range-dependent water column sound speed profiles on the New Jersey shelf using a linearized
Megan S Ballard1, Kyle M Becker
1Applied Research Laboratories, University of Texas at Austin, Texas 78758, USA. meganb@arlut.utexas.edu
Abstract:
The environment of the New Jersey shelf is characterized by high spatial and temporal variability of water column properties caused by intrusions of warm, salty water from the continental slope. These intrusions cause fluctuations in the water column sound speed profile which can have significant effects on acoustic propagation in shallow water. In this work, a linearized perturbative inverse technique is applied to estimate range-dependent water column sound speed profiles. This method utilizes estimates of horizontal wave numbers to determine sound speed as a function of depth. This technique is appropriate for the range-dependent shallow-water environment as horizontal wave numbers can be measured semilocally (1-2 km aperture) and their values are a direct measurement of the local environmental parameters. Difficulty is encountered in application of the perturbative inverse technique because the wave number data are insensitive to some portions of the waveguide and, as a result, the solution can deviate wildly from true values. This issue is addressed by application of approximate equality constraints which force the solution to be close to likely values at prescribed locations.
Related Concept Videos
Deriving the Speed of Sound in a Liquid
The speed of sound in fluids can be derived by considering a mechanical wave propagating...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
Speed of Sound in Solids and Liquids
Standing Waves in a Cavity
Newtonian Fluid: Problem Solving
A velocity gradient forms within the fluid when a Newtonian fluid is placed between two parallel plates, with...
Bernoulli's Equation for Flow Along a Streamline

