The Antarctic Slope Current near 30 degrees E
The Antarctic Slope Current flows westward above the continental slope of Antarctica, entering the Weddell Sea near 30 degrees E and supplying dense water to the deep overturning cell there, and contributing to global Antarctic Bottom Water formation. Observations from the 2008 I6S hydrographic sect...
Other Authors: | , , |
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Format: | Text |
Language: | English |
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2016
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Online Access: | https://diginole.lib.fsu.edu/islandora/object/fsu%3A405767/datastream/TN/view/The%20Antarctic%20Slope%20Current%20near%2030%20degrees%20E.jpg |