Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations

Abstract It has been suggested that the Atlantic meridional overturning circulation (AMOC) in many CMIP6 models is overly sensitive to anthropogenic aerosol forcing, and it has been proposed that this is due to the inclusion of aerosol indirect effects for the first time in many CMIP6 models. We ana...

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Published in:Geophysical Research Letters
Main Authors: Michael R. Needham, Douglas D. Falter, David A. Randall
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:https://doi.org/10.1029/2023GL106410
https://doaj.org/article/a495c650de784eab853356475aae7e65
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spelling ftdoajarticles:oai:doaj.org/article:a495c650de784eab853356475aae7e65 2024-09-09T19:57:09+00:00 Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations Michael R. Needham Douglas D. Falter David A. Randall 2024-03-01T00:00:00Z https://doi.org/10.1029/2023GL106410 https://doaj.org/article/a495c650de784eab853356475aae7e65 EN eng Wiley https://doi.org/10.1029/2023GL106410 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106410 https://doaj.org/article/a495c650de784eab853356475aae7e65 Geophysical Research Letters, Vol 51, Iss 5, Pp n/a-n/a (2024) AMOC aerosol‐cloud‐climate interactions CESM large ensembles poleward energy transport Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2023GL106410 2024-08-05T17:49:23Z Abstract It has been suggested that the Atlantic meridional overturning circulation (AMOC) in many CMIP6 models is overly sensitive to anthropogenic aerosol forcing, and it has been proposed that this is due to the inclusion of aerosol indirect effects for the first time in many CMIP6 models. We analyze the AMOC response in a newly released ensemble of simulations performed with CESM2 forced by the CMIP5 input data sets (CESM2‐CMIP5). This AMOC response is then compared to the CMIP5‐generation CESM1 large ensemble (CESM1‐LE) and the CMIP6‐generation CESM2 large ensemble (CESM2‐LE). A key conclusion, only made possible by this experimental setup, is that changes in aerosol‐indirect effects cannot explain differences in AMOC response between CESM1‐LE and CESM2‐LE. Instead, we hypothesize that the difference is due to increased interannual variability of anthropogenic emissions. This forcing variability may act through a nonlinear relationship between the surface heat budget of the North Atlantic and the AMOC. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 51 5
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic AMOC
aerosol‐cloud‐climate interactions
CESM
large ensembles
poleward energy transport
Geophysics. Cosmic physics
QC801-809
spellingShingle AMOC
aerosol‐cloud‐climate interactions
CESM
large ensembles
poleward energy transport
Geophysics. Cosmic physics
QC801-809
Michael R. Needham
Douglas D. Falter
David A. Randall
Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
topic_facet AMOC
aerosol‐cloud‐climate interactions
CESM
large ensembles
poleward energy transport
Geophysics. Cosmic physics
QC801-809
description Abstract It has been suggested that the Atlantic meridional overturning circulation (AMOC) in many CMIP6 models is overly sensitive to anthropogenic aerosol forcing, and it has been proposed that this is due to the inclusion of aerosol indirect effects for the first time in many CMIP6 models. We analyze the AMOC response in a newly released ensemble of simulations performed with CESM2 forced by the CMIP5 input data sets (CESM2‐CMIP5). This AMOC response is then compared to the CMIP5‐generation CESM1 large ensemble (CESM1‐LE) and the CMIP6‐generation CESM2 large ensemble (CESM2‐LE). A key conclusion, only made possible by this experimental setup, is that changes in aerosol‐indirect effects cannot explain differences in AMOC response between CESM1‐LE and CESM2‐LE. Instead, we hypothesize that the difference is due to increased interannual variability of anthropogenic emissions. This forcing variability may act through a nonlinear relationship between the surface heat budget of the North Atlantic and the AMOC.
format Article in Journal/Newspaper
author Michael R. Needham
Douglas D. Falter
David A. Randall
author_facet Michael R. Needham
Douglas D. Falter
David A. Randall
author_sort Michael R. Needham
title Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
title_short Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
title_full Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
title_fullStr Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
title_full_unstemmed Changes in External Forcings Drive Divergent AMOC Responses Across CESM Generations
title_sort changes in external forcings drive divergent amoc responses across cesm generations
publisher Wiley
publishDate 2024
url https://doi.org/10.1029/2023GL106410
https://doaj.org/article/a495c650de784eab853356475aae7e65
genre North Atlantic
genre_facet North Atlantic
op_source Geophysical Research Letters, Vol 51, Iss 5, Pp n/a-n/a (2024)
op_relation https://doi.org/10.1029/2023GL106410
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL106410
https://doaj.org/article/a495c650de784eab853356475aae7e65
op_doi https://doi.org/10.1029/2023GL106410
container_title Geophysical Research Letters
container_volume 51
container_issue 5
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