Water Mass Exchange Between the Weddell Gyre and the Antarctic Circumpolar Current
The Weddell Sea is a primary bottom water formation region, where newly formed bottom water is exported to all the ocean basins. This water mass is partly supplied from the upper layers of the Antarctic Circumpolar Current (ACC), as well as from sources within the Antarctic Slope Current (ASC). In a...
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Format: | Text |
Language: | English |
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Florida State University
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Online Access: | http://purl.flvc.org/fsu/fd/FSU_migr_etd-5344 http://fsu.digital.flvc.org/islandora/object/fsu%3A183240/datastream/TN/view/Water%20Mass%20Exchange%20Between%20the%20Weddell%20Gyre%20and%20the%20Antarctic%20Circumpolar%20Current.jpg |