nerc.ac.uk

The role of anthropogenic aerosol forcing in the 1850–1985 strengthening of the AMOC in CMIP6 historical simulations

Robson, Jon; Menary, Matthew B.; Sutton, Rowan T.; Mecking, Jenny; Gregory, Jonathan M.; Jones, Colin; Sinha, Bablu; Stevens, David P.; Wilcox, Laura J.. 2022 The role of anthropogenic aerosol forcing in the 1850–1985 strengthening of the AMOC in CMIP6 historical simulations. Journal of Climate, 35 (20). 3243-3263. https://doi.org/10.1175/JCLI-D-22-0124.1

Before downloading, please read NORA policies.
[img]
Preview
Text
1520-0442-JCLI-D-22-0124.1.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (5MB) | Preview

Abstract/Summary

Previous work has shown that anthropogenic aerosol (AA) forcing drives a strengthening in the Atlantic meridional overturning circulation (AMOC) in CMIP6 historical simulations over 1850–1985, but the mechanisms have not been fully understood. Across CMIP6 models, it is shown that there is a strong correlation between surface heat loss over the subpolar North Atlantic (SPNA) and the forced strengthening of the AMOC. Despite the link to AA forcing, the AMOC response is not strongly related to the contribution of anomalous downwelling surface shortwave radiation to SPNA heat loss. Rather, the spread in AMOC response is primarily due to the spread in turbulent heat loss. We hypothesize that turbulent heat loss is larger in models with strong AA forcing because the air advected over the ocean is colder and drier, in turn because of greater AA-forced cooling over the continents upwind, especially North America. The strengthening of the AMOC also feeds back on itself positively in two distinct ways: by raising the sea surface temperature and hence further increasing turbulent heat loss in the SPNA, and by increasing the sea surface density across the SPNA due to increased northward transport of saline water. A comparison of key indices suggests that the AMOC response in models with strong AA forcing is not likely to be consistent with observations.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1175/JCLI-D-22-0124.1
ISSN: 0894-8755
Date made live: 22 Nov 2022 14:46 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/533602

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...