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...

Full description

Bibliographic Details
Published in:Science Advances
Main Authors: Ohshima, Kay I., Fukamachi, Yasushi, Ito, Masato, Nakata, Kazuki, Simizu, Daisuke, Ono, Kazuya, Nomura, Daiki, Hashida, Gen, Tamura, Takeshi
Format: Article in Journal/Newspaper
Language:English
Published: The American Association for the Advancement of Science(AAAS)
Subjects:
452
Online Access:http://hdl.handle.net/2115/87550
https://doi.org/10.1126/sciadv.adc9174