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March 27, 2025

Voyage tracks some of the world's fiercest ocean currents in the Mozambique Channel

The movement of ocean chlorophyll (green) in the Mozambique Channel in April 2022 is depicted here. A large anticyclonic ring (dark blue coloration near the top of the image) pulls a chlorophyll-rich water filament into the channel from the coast, while another filament spirals into a smaller cyclonic eddy to the south. Credit: Pierrick Penven
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The movement of ocean chlorophyll (green) in the Mozambique Channel in April 2022 is depicted here. A large anticyclonic ring (dark blue coloration near the top of the image) pulls a chlorophyll-rich water filament into the channel from the coast, while another filament spirals into a smaller cyclonic eddy to the south. Credit: Pierrick Penven

The Mozambique Channel, between Mozambique and Madagascar, is home to some of the most turbulent waters in the ocean. Swirling at a rate of more than 1 meter per second, currents in the channel can form structures known as anticyclonic rings that spread up to 350 kilometers across—about the width of Missouri—and extend 2,000 meters below the surface.

The currents carry nutrients and such as shrimp larvae, the basis of a major industry in Mozambique. Information about the movements of shrimp larvae and their food is crucial for managing fisheries. Yet currents in the Mozambique Channel remain poorly understood.

Pierrick Penven and colleagues have characterized currents in the channel as part of a study called RESILIENCE (Fronts, Eddies, and Marine Life in the Western Indian Ocean). In 2022, the research team set off aboard a vessel towing a Moving Vessel Profiler, which measured water conductivity, temperature, and turbidity in the region with unprecedented spatial resolution. Meanwhile, an instrument on the ship's hull, called the RDI Ocean Surveyor Acoustic Doppler Current Profiler, measured water velocity.

Specifically, the researchers traversed a prominent type of in the Mozambique Channel known as an eddy-ring dipole. In an eddy-ring dipole, an anticyclonic ring—in which water swirls counterclockwise in the Southern Hemisphere—pairs with a cyclonic eddy—in which water swirls clockwise in the Southern Hemisphere. Using the profiling instruments, the team took high-resolution measurements of several cross-sections of the current down to a depth of 300 meters.

The fierce central current formed by the eddy-ring dipole whisked nutrients and sea life away from the and the Mozambican coast at speeds of up to 1.3 meters per second, the researchers found. They also found that conditions vary significantly between the current's two parts. In the cyclonic eddy, patches of either high or low salinity exist and photosynthetic life is abundant. In the anticyclonic ring, on the other hand, conditions are homogeneous and photosynthetic life is largely absent.

The study is among the first to characterize these complex currents, and it provides a basis for future research on this turbulent region, the researchers say. The work is in the Journal of Geophysical Research: Oceans.

More information: Pierrick Penven et al, Characterizing the Central Structure of a Mesoscale Eddy‐Ring Dipole in the Mozambique Channel From In Situ Observations, Journal of Geophysical Research: Oceans (2025).

Journal information: Journal of Geophysical Research

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The Mozambique Channel features some of the ocean's most turbulent currents, forming anticyclonic rings up to 350 km wide and 2,000 m deep. These currents transport nutrients and marine life, crucial for Mozambique's shrimp industry. High-resolution measurements revealed an eddy-ring dipole, with distinct conditions in its cyclonic and anticyclonic parts, affecting nutrient and marine life distribution. This research enhances understanding of these complex currents.

This summary was automatically generated using LLM.