Antarctic Bottom Water production by intense sea-ice formation in the Cape Darnley polynya
The formation of Antarctic Bottom Water—the cold, dense water that occupies the abyssal layer of the global ocean—is a key process in global ocean circulation. This water mass is formed as dense shelf water sinks to depth. Three regions around Antarctica where this process takes place have been prev...
Published in: | Nature Geoscience |
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Main Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2013
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Subjects: | |
Online Access: | https://eprints.soton.ac.uk/398666/ |