Dominant frazil ice production in the Cape Darnley polynya leading to Antarctic Bottom Water formation
Antarctic Bottom Water (AABW) occupies the abyssal layer of the world ocean and contributes to the global over-turning circulation. It originates from dense shelf water, which forms from brine rejection during sea ice production. An important region of AABW formation has been identified off the Cape...
Published in: | Science Advances |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The American Association for the Advancement of Science(AAAS)
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Subjects: | |
Online Access: | http://hdl.handle.net/2115/87550 https://doi.org/10.1126/sciadv.adc9174 |