The Mozambique Channel is home to turbulent waters driven by mesoscale eddies that impact local biodiversity, sediment mixing, and plastic pollution movement.
Scientists measured a mesoscale dipole in the region, which consisted of a large counterclockwise anticyclonic ring and a smaller clockwise cyclonic eddy.
The anticyclonic ring had uniform waters with low chlorophyll, while the cyclonic eddy had high chlorophyll levels and varying salinity, driving vertical motions up to 40 meters per day.
In situ measurements like these aid in understanding energy flows in the ocean, guiding predictions related to nutrient transport, sediment movement, and the impact of climate patterns on the region.