Observations of Double Diffusive Staircase Edges in the Arctic Ocean
Recent observational studies have provided detailed descriptions of double‐diffusive staircases in the Beaufort Sea, characterized by well‐mixed intrusions between high‐gradient interfaces. These structures result from double‐diffusive convection, occurring when cooler fresh water lies atop the warm...
| Main Authors: | , , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
American Geophysical Union
2024
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| Subjects: | |
| Online Access: | https://hdl.handle.net/1721.1/154058 |