Warming Trend in Antarctic Bottom Water in the Vema Channel in the South Atlantic.

Campos, Edmo J. D. , Caspel, Mathias C., Zenk, Walter, Morozov, Eugene G. , Frey, Dmitry I. , Piola, Alberto R. , Meinen, Christopher S. , Sato, Olga T. , Perez, Renellys C. and Dong, Shenfu (2021) Warming Trend in Antarctic Bottom Water in the Vema Channel in the South Atlantic. Open Access Geophysical Research Letters, 48 (19). Art.Nr. e2021GL094709. DOI 10.1029/2021GL094709.

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Abstract

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 linked to changes in the Weddell Sea. We present a new moored temperature time series sampled near the bottom in the Vema Channel, from February 2019 to August 2020. Together with historical data, the combined record confirms the warming of the abyssal waters, with an increase of 0.059°C in potential temperature between January 1991 and August 2020, embedded within intense high-frequency variability. Moreover, the data suggest the possibility of an accelerated warming, with a change in the temperature trend from 0.0016°C yr−1, between the early 1990s and 2005, to 0.0026°C yr−1 afterwards.

Document Type: Article
Keywords: AABW Warming Trend; South Atlantic; Vema Channel
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-PO Physical Oceanography
HGF-AWI
Main POF Topic: PT2: Ocean and Cryosphere
Refereed: Yes
Open Access Journal?: No
Publisher: AGU (American Geophysical Union), Wiley
Projects: WOCE, CLIVAR
Date Deposited: 25 Oct 2021 08:20
Last Modified: 07 Feb 2024 15:46
URI: https://oceanrep.geomar.de/id/eprint/54268

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