Irminger Rings are mesoscale oceanic features that occur in the Irminger Sea, located to the southwest of Greenland. These rings are formed from the dynamics of ocean currents and temperature gradients and are associated with the North Atlantic Ocean's circulation patterns. Key characteristics of Irminger Rings include: 1. **Formation**: They are typically formed from the interaction of warm, saline water from the Atlantic Ocean with colder, fresher water from the Arctic region.
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