Mechanisms of the overturning circulation in the northern Red Sea other than convective mixing
Lina Eyouni,Zoi Kokkini,Nikolaos D. Zarokanellos,and Burton H. Jones
Lina Eyouni
Biological and Environmental Sciences and Engineering (BESE), Red Sea Research Center (RSRC), King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
Biological and Environmental Sciences and Engineering (BESE), Red Sea Research Center (RSRC), King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
Institute of Marine Sciences, National Research Council of Italy (CNR-ISMAR), Pozzuolo di Lerici, Italy
Biological and Environmental Sciences and Engineering (BESE), Red Sea Research Center (RSRC), King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
Balearic Islands Coastal Observing and Forecasting System (SOCIB), Palma de Mallorca, Spain
Biological and Environmental Sciences and Engineering (BESE), Red Sea Research Center (RSRC), King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
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Total article views: 2,951 (including HTML, PDF, and XML)
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This study examines how multiple processes in the northern Red Sea form Red Sea Outflow Water and affect biogeochemical fluxes. Using glider data, wind and air–sea flux reanalysis, and satellite observations, it highlights seasonal evolution. Eddy-driven upwelling exposes cool water to heat loss and evaporation, fueling primary productivity. Circulation patterns block inflows, extend cooling, and subduct water into the ocean interior, influencing regional dynamics.
This study examines how multiple processes in the northern Red Sea form Red Sea Outflow Water...