🎙️ How desalination is reshaping the Arabian Gulf – listen now.

Khalifa University researchers find that desalination is reshaping the Arabian Gulf’s ocean circulation.
By 2050, desalination capacity in the Arabian Gulf is projected to increase more than sixfold. The discharge from these plants, a denser brine that is saltier and often warmer than ambient seawater, sinks and spreads along the seafloor. A new modeling study from Khalifa University’s Dr. Maryam Al Shehhi and Fahim Abdul Gafoor, with researchers from MIT and Yonsei University, Republic of Korea, explores the oceanographic costs of this brine. The results were published in and the results are clear: desalination alters local salinity and flow patterns significantly, but the Gulf’s natural dynamics may prevent the worst large-scale impacts, at least for now.
Using a high-resolution ocean model, the study simulated a range of desalination scenarios from none to a hypothetical 50-fold increase over current levels. In the most extreme scenario, bottom salinity near the southern coast increased by more than 2g/kg, and temperatures rose by 0.6C. These changes triggered shifts in local currents: fresher surface water was drawn towards desalination sites, while dense salty water sank and flowed out of the Gulf through the Strait of Hormuz. The study found a 20 percent increase in both inflow and outflow rates through the strait, strengthening the Gulf’s overturning circulation in both horizontal and vertical planes.
“The Arabian Gulf’s natural circulation offers a strong buffer against large-scale salinity buildup from desalination plants, but the risk to coastal ecosystems near the plants remains significant.”
— Assistant Professor Maryam Al Shehhi, Khalifa University.
These changes are largely driven by density differences created by brine discharge. This mechanism not only alters local flow but also reinforces the Gulf’s natural exchange with the Sea of Oman. Despite significant local impacts, the researchers found that the Gulf’s basin-wide temperature and salinity remain relatively stable, thanks to this efficient exchange.
The study also ݮƵ that the brine discharge enhances water mass transformation processes within the Gulf. These shifts could have longer-term implications for marine ecosystems, especially if combined with warming from climate change or further expansion of desalination infrastructure. The researchers caution that their findings represent upper-bound impacts, based on assumptions of uniform brine recovery and idealized plant distributions.
Jade Sterling
Science Writer