Lagrangian decomposition of the Atlantic Ocean heat transport at 26.5°N
Tooth, Oliver J.; Foukal, Nicholas P.; Johns, William E.; Johnson, Helen L.; Wilson, Chris ORCID: https://orcid.org/0000-0003-0891-2912. 2024 Lagrangian decomposition of the Atlantic Ocean heat transport at 26.5°N. Geophysical Research Letters, 51 (14). 10.1029/2023GL107399
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Geophysical Research Letters - 2024 - Tooth - Lagrangian Decomposition of the Atlantic Ocean Heat Transport at 26 5 N.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (2MB) | Preview |
Abstract/Summary
The Atlantic Meridional Overturning Circulation (AMOC) plays a critical role in the global climate system through the redistribution of heat, freshwater and carbon. At 26.5°N, the meridional heat transport has traditionally been partitioned geometrically into vertical and horizontal circulation cells; however, attributing these components to the AMOC and Subtropical Gyre (STG) flow structures remains widely debated. Using water parcel trajectories evaluated within an eddy-rich ocean hindcast, we present the first Lagrangian decomposition of the meridional heat transport at 26.5°N. We find that water parcels recirculating within the STG account for 37% (0.36 PW) of the total heat transport across 26.5°N, more than twice that of the classical horizontal gyre component (15%). Our findings indicate that STG heat transport cannot be meaningfully distinguished from that of the basin-scale overturning since water parcels cooled within the gyre subsequently feed the northward, subsurface limb of the AMOC.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1029/2023GL107399 |
ISSN: | 0094-8276 |
Additional Keywords: | Lagrangrian trajectories, meridional heat transport, RAPID 26.5N, subtropical gyre, Atlantic meridional overturning circulation |
Date made live: | 24 Jul 2024 12:38 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/537761 |
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