with antarctic bottom water formation considered to be active in the western perimeter of the Weddell gyre and near the gyre center just to the west of Maud Rise. The warm-saline deep water is advected to the west of

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Date: 2011-05-06 06:43:22 Oceanic gyres Filchner-Ronne Ice Shelf Argentine Antarctica Weddell Gyre Weddell Sea Ocean gyre Antarctic Bottom Water Expendable bathythermograph USNS Eltanin Physical geography Oceanography Physical oceanography		with antarctic bottom water formation considered to be active in the western perimeter of the Weddell gyre and near the gyre center just to the west of Maud Rise. The warm-saline deep water is advected to the west of Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 1,92 MB Share Document on Facebook

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