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...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Campos, Edmo, van Caspel, Mathias C., Zenk, Walter, Morozov, Eugene G., Frey, Dmitry I., Piola, Alberto Ricardo, Meinen, Christopher S., Sato, Olga T., Perez, Renellys C., Dong, Shenfu
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
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Online Access:http://hdl.handle.net/11336/166547