
Journal of Geophysical Research Oceans, Journal Year: 2025, Volume and Issue: 130(3)
Published: March 1, 2025
Abstract During the RESILIENCE cruise aboard R/V Marion Dufresne II (April 19–24 May 2022), a high‐resolution in situ observation campaign investigated mesoscale dipole Mozambique Channel, composed of large anticyclonic ring and cyclonic eddy. Using an innovative adaptive sampling strategy to track its movement, we employed continuous observing systems, including Moving Vessel Profiler Acoustic Doppler Current Profilers, capture vertical sections. The results revealed distinct dipolar structure: 250 km‐wide featured low chlorophyll homogeneous waters, while smaller eddy exhibited higher concentrations pronounced salinity variations. These include patches, vertically stacked layers, filaments, reflecting mix contrasted water masses from southern Channel Sofala Bank. A central jet between eddies horizontal velocities up 130 cm , facilitating significant offshore transport exceeding 10 Sverdrups upper m emphasizing dipole's role eastward movement. Vertical velocities, derived Quasi‐Geostrophic Omega equation, highlighted influence smaller‐scale structures driving motions, reaching 40 at depth. Lagrangian particle trajectories spiraling structure connectivity coastal waters. findings show that Eddy‐Ring Dipoles efficiently properties continental shelf open ocean, enhancing regional ecosystem connectivity. This work provides new insights into their biogeochemical, biological ecological significance, challenging traditional cyclonic/anticyclonic paradigms, setting foundation for future studies on dipoles region.
Language: Английский