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Signal and noise in the Atlantic Meridional Overturning Circulation at 26°N

McCarthy, Gerard D. ORCID: https://orcid.org/0000-0002-2363-0561; Hug, Guillaume ORCID: https://orcid.org/0009-0009-7343-6562; Smeed, David ORCID: https://orcid.org/0000-0003-1740-1778; Morris, Kirsty J.; Moat, Ben ORCID: https://orcid.org/0000-0001-8676-7779. 2025 Signal and noise in the Atlantic Meridional Overturning Circulation at 26°N. Geophysical Research Letters, 52 (7). 10.1029/2025GL115055

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© 2025 The Author(s).This is an open access article under the terms of the Creative Commons Attribution‐Non Commercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
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Abstract/Summary

The Atlantic meridional overturning circulation (AMOC) plays a crucial role in redistributing heat within the climate system. The RAPID mooring array has observed an AMOC weakening of 1.0 [0.4–1.6] Sv per decade from 2004 to 2023, consistent with climate model projections and not consistent with a collapse in the mid-21st century. Here, we analyze the AMOC change within a signal-to-noise framework. We find a strong signal in Lower North Atlantic Deep Water (LNADW) and thermocline transports. By removing the influence of Ekman transport on AMOC and LNADW estimates, we reduce noise by 30% and 22%, respectively. Moreover, we demonstrate that a simple model of LNADW yields a comparable signal-to-noise ratio to the full AMOC estimate. Ultimately, we conclude that current AMOC trends are unlikely to reach “unfamiliar” (signal-to-noise ratio > 2) or “unknown” (signal-to-noise ratio > 3) thresholds until the 2040s and 2060s, respectively.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1029/2025GL115055
ISSN: 0094-8276
Additional Keywords: meridional overturning circulation, rapid climate change, ocean observing systems, detection of climate change, deep circulation, ocean variability
Date made live: 01 Apr 2025 13:52 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/539195

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