Global oceans - Meridional overturning circulation and heat transport in the Atlantic Ocean [in: State of the Climate in 2023]
Volkov, D. L.; Willis, J. K.; Hobbs, W.; Fu, Y.; Lozier, S. M.; Johns, W. E.; Smeed, D. A. ORCID: https://orcid.org/0000-0003-1740-1778; Moat, B. I. ORCID: https://orcid.org/0000-0001-8676-7779; Pita, I.; Goes, M.; Dong, S.; Smith, R. H.; Elipot, S.. 2024 Global oceans - Meridional overturning circulation and heat transport in the Atlantic Ocean [in: State of the Climate in 2023]. Bulletin of the American Meteorological Society, 105 (8). S191. 10.1175/BAMS-D-24-0100.1
Full text not available from this repository.Abstract/Summary
The meridional overturning circulation (MOC) and meridional heat transport (MHT) are essential indicators of the state of the large-scale ocean circulation and Earth’s climate system. Most climate models and proxy-based reconstructions indicate that the Atlantic MOC may already be slowing down towards the end of this century in response to anthropogenic forcing (Weijer et al. 2020; Rahmstorf et al. 2015; Caesar et al. 2018, 2021). In this report, we provide updates on the MOC/MHT estimates across the Atlantic Ocean from the following observing platforms: 1) the Overturning in the Subpolar North Atlantic Program (OSNAP) array (Lozier et al. 2017), which consists of a West section from Canada to Greenland across the Labrador Sea and an East section from Greenland to Scotland, 2) the RAPID-Meridional Overturning Circulation and Heat-flux Array - Western Boundary Time Series (henceforth RAPID) array at ~26.5°N (Moat et al. 2023), and 3) from the combination of satellite and in situ data (synthetic MOC/MHT) at 41°N and at several latitudes in the South Atlantic (Fig. 3.21). As a highlight of this report, initial estimates indicate a record-high MOC/MHT at 41°N, albeit over a short (20-year) observational record.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1175/BAMS-D-24-0100.1 |
ISSN: | 0003-0007 |
Date made live: | 10 Oct 2024 12:44 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/538214 |
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