SOFAR Channel Sound Speed Calculator
Physical oceanography & underwater acoustics: Compute seawater sound velocity profiles (Mackenzie 9-term equation), SOFAR channel waveguide axis, and ray bending curvature.
Ocean Hydrographic Parameters
Acoustic Propagation & Waveguide Analysis
Recommended Tools & Equipment
Tested hardware and components for high reliability
Frequently Asked Questions
Why does sound speed reach a minimum at the SOFAR axis?
Sound speed in seawater depends primarily on temperature, salinity, and pressure. Near the surface, temperature drops steeply through the main thermocline, causing sound speed to decrease. At greater depths, temperature is nearly constant, but hydrostatic pressure increases steadily, driving sound speed upward. The balance creates an acoustic minimum known as the SOFAR axis.
How does Snell law explain ray bending in seawater?
Because sound speed varies with depth, the wavefront travels faster in the higher-speed region, causing the wave vector to turn toward the lower sound speed region. Acoustic energy is continuously focused back toward the sound channel axis.
What is the practical use of the SOFAR channel?
The SOFAR channel is utilized for global ocean acoustic tomography, hydroacoustic monitoring of clandestine nuclear tests (CTBTO IMS network), long-range underwater navigation for autonomous underwater vehicles (AUVs), and marine mammal bioacoustic tracking.