Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect

Effective climate sensitivity (EffCS), commonly estimated from model simulations with abrupt 4xCO(2) for 150 years, has been shown to depend on the CO2 forcing level. To understand this dependency systematically, we performed a series of simulations with a range of abrupt CO2 forcing in two climate...

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Published in:Geophysical Research Letters
Other Authors: Mitevski, Ivan (author), Dong, Yue (author), Polvani, Lorenzo M. (author), Rugenstein, Maria (author), Orbe, Clara (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL103617
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spelling ftncar:oai:drupal-site.org:articles_26502 2023-10-01T03:57:45+02:00 Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect Mitevski, Ivan (author) Dong, Yue (author) Polvani, Lorenzo M. (author) Rugenstein, Maria (author) Orbe, Clara (author) 2023-07-28 https://doi.org/10.1029/2023GL103617 en eng Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007 articles:26502 doi:10.1029/2023GL103617 ark:/85065/d7rn3cwv Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2023 ftncar https://doi.org/10.1029/2023GL103617 2023-09-04T18:18:44Z Effective climate sensitivity (EffCS), commonly estimated from model simulations with abrupt 4xCO(2) for 150 years, has been shown to depend on the CO2 forcing level. To understand this dependency systematically, we performed a series of simulations with a range of abrupt CO2 forcing in two climate models. Our results indicate that normalized EffCS values in these simulations are a non-monotonic function of the CO2 forcing, decreasing between 3x and 4xCO(2) in CESM1-LE (2x and 3xCO(2) in GISS-E2.1-G) and increasing at higher CO2 levels. The minimum EffCS value, caused by anomalously negative radiative feedbacks, arises mainly from sea-surface temperature (SST) relative cooling in the tropical and subtropical North Atlantic. This cooling is associated with the formation of the North Atlantic Warming Hole and Atlantic Meridional Overturning Circulation collapse under CO2 forcing. Our findings imply that understanding changes in North Atlantic SST patterns is important for constraining near-future and equilibrium global warming. Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Geophysical Research Letters 50 14
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Effective climate sensitivity (EffCS), commonly estimated from model simulations with abrupt 4xCO(2) for 150 years, has been shown to depend on the CO2 forcing level. To understand this dependency systematically, we performed a series of simulations with a range of abrupt CO2 forcing in two climate models. Our results indicate that normalized EffCS values in these simulations are a non-monotonic function of the CO2 forcing, decreasing between 3x and 4xCO(2) in CESM1-LE (2x and 3xCO(2) in GISS-E2.1-G) and increasing at higher CO2 levels. The minimum EffCS value, caused by anomalously negative radiative feedbacks, arises mainly from sea-surface temperature (SST) relative cooling in the tropical and subtropical North Atlantic. This cooling is associated with the formation of the North Atlantic Warming Hole and Atlantic Meridional Overturning Circulation collapse under CO2 forcing. Our findings imply that understanding changes in North Atlantic SST patterns is important for constraining near-future and equilibrium global warming.
author2 Mitevski, Ivan (author)
Dong, Yue (author)
Polvani, Lorenzo M. (author)
Rugenstein, Maria (author)
Orbe, Clara (author)
format Article in Journal/Newspaper
title Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
spellingShingle Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
title_short Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
title_full Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
title_fullStr Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
title_full_unstemmed Non-monotonic feedback dependence under abrupt CO2 forcing due to a North Atlantic pattern effect
title_sort non-monotonic feedback dependence under abrupt co2 forcing due to a north atlantic pattern effect
publishDate 2023
url https://doi.org/10.1029/2023GL103617
genre North Atlantic
genre_facet North Atlantic
op_relation Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007
articles:26502
doi:10.1029/2023GL103617
ark:/85065/d7rn3cwv
op_rights Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
op_doi https://doi.org/10.1029/2023GL103617
container_title Geophysical Research Letters
container_volume 50
container_issue 14
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