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: | Boury, S., Supekar, R., Fine, E. C., Musgrave, R., Mickett, J. B., Voet, G., Odier, P., Peacock, T., MacKinnon, J. A., Alford, M. H. |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Mechanical Engineering |
Format: | Article |
Language: | English |
Published: |
American Geophysical Union
2024
|
Subjects: | |
Online Access: | https://hdl.handle.net/1721.1/154058 |
Similar Items
-
Frontal Dynamics in the Alboran Sea: 2. Processes for Vertical Velocities Development
by: Garcia‐Jove, Maximo, et al.
Published: (2024) -
The “Polar Vortex” Winter of 2013/2014
by: Cohen, Judah, et al.
Published: (2023) -
Structural relationships and geochemical investigation of the Lynn Volcanic Complex, Pine Hill, Boston North Quadrangle, Massachusetts.
by: Zarrow, Lorraine
Published: (2010) -
The marine geochemistry of methane.
by: Scranton, Mary Isabelle
Published: (2006) -
Geochemistry of Eyjafjöll, a volcano in Southern Iceland.
by: Arney, Barbara Holota
Published: (2011)