Warming trend in Antarctic Bottom Water in the Vema Channel in the South Atlantic
The excess heat absorbed from the atmosphere has increased the temperature in the upper layers of the ocean (<2,000 m). In the abyss, infrequently repeated ship sections, deep Argo float measurements, and sparse moored observations have found signs of warming in the Southwest Atlantic, possibly l...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/11336/166547 |