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Multibeam Swath Bathymetry in Arabian Gulf Waters: Solving Sound Velocity & Halocline Challenges

Technical analysis of extreme salinity (42-46 PSU) and thermal stratification in the Jubail and Dammam coastal basins, and why dual-hourly SVP profiling is critical to meet IHO S-44 Special Order soundings.

person Hydrographic Compliance Directorate schedule 7 min read calendar_today September 11, 2026
Multibeam Swath Bathymetry in Arabian Gulf Waters: Solving Sound Velocity & Halocline Challenges

The Oceanographic Environment of the Arabian Gulf

The Arabian Gulf represents one of the most chemically and thermally demanding marine environments for acoustic hydrography anywhere in the world. Being an enclosed, shallow marginal sea subjected to hyper-arid desert evaporation, salinity levels in coastal basins like Jubail Industrial City, Ras Tanura, and Tarut Bay routinely surge to between 42 and 46 PSU (Practical Salinity Units)—compared to global oceanic averages of 35 PSU.

In addition, heavy petrochemical cooling water outfalls create sharp localized thermal plumes, where sea surface temperatures fluctuate from 16°C in winter to over 36°C in late summer.


The Acoustic Ray Bending Problem

Because salinity and temperature form steep haloclines and thermoclines within the top 5 to 15 meters, acoustic rays refract significantly according to Snell's Law. Without real-time sound velocity profiling (SVP), outer beams of a multibeam swath suffer vertical sounding errors exceeding 0.40 m—instantly failing IHO S-44 Special Order requirements (0.15 m maximum total vertical uncertainty).


Mandatory Hydrographic Protocol for Jubail & Eastern Province

To guarantee full compliance with Saudi Ports Authority (Mawani) and RCJY standards:

  1. Real-time Surface Sound Velocity: Continuous SVP probe mounted directly at the sonar transducer face.
  2. Periodic Full-Column SVP Casts: Automated profiling winches deploying Valeport or AML probes every 120 minutes.
  3. Co-Tidal Corrections: Dual-frequency tide gauge stations linked to the Ras Abu Ali co-tidal model.