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Ocean science· 2026Q1

Hydrographic transformation of the Persian/Arabian Gulf outflow over rough shelf bathymetry in the Gulf of Oman

Ahmed J. Abdelmaksoud, Aisha Al Suwaidi, Gerd Bruss, Kaveh Samimi‐Namin et al.

Short summary

Rough shelf bathymetry in the Gulf of Oman causes the hypersaline Persian/Arabian Gulf outflow to thicken, lose bottom contact, and mix significantly, altering its properties and impacting the Arabian Sea's Oxygen Minimum Zone.

AI-generated from the title and abstract; the full text is not read.

Key points

  • Rough shelf bathymetry in the Gulf of Oman causes the Persian/Arabian Gulf outflow to thicken and detach from the seafloor.
  • Downstream, the outflow experiences enhanced mixing, leading to decreased salinity, oxygen, and pH.
  • Distinct benthic communities are associated with attached versus detached flow sectors, indicating differing hydrodynamic regimes.
  • Bathymetric roughness is the primary control on the near-field transformation of the outflow.

AI-generated from the title and abstract; the full text is not read.

Abstract

Abstract. Hypersaline overflows from Marginal seas contribute to global ocean circulation and climate variability. The Persian/Arabian Gulf (P/AG) contributes dense, saline, oxygenated deep outflow into the Arabian Sea’s Oxygen Minimum Zone (OMZ). Here, we present high-resolution hydrographic mapping of the UAE-Oman margin in the northwestern Arabian Sea, integrating CTD profiles, multibeam bathymetry and ROV imagery. The P/AG outflow forms a thin bottom-attached layer that thickens dramatically over the rough, irregular seafloor of the unstable shelf, where dilution and loss of bottom contact occur. Near-bottom salinity, oxygen, and pH decrease systematically downstream in association with enhanced mixing. Distinct benthic assemblages coincide with attached versus detached flow sectors, consistent with differing near-bed hydrodynamic regimes. These observations indicate that bathymetric roughness controls the near-field transformation of the outflow. Because outflow density depends on Gulf warming and evaporation, modest climatic shifts may alter detachment depth, pathway geometry, and intermediate-depth ventilation of the Arabian Sea OMZ.

The authors' abstract, as published at the source. Ocean science, 2026 · DOI ↗

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OceanographyEarth and Planetary Sciences