Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing
In this thesis, I explore the climate system's response to symmetric abrupt and transient CO₂ forcing across a range of concentrations, from ⅛ ⨉ to 8⨉CO₂, relative to pre-industrial levels. I use two CMIP6 class models: the CESM Large Ensemble (CESM-LE) model configuration and the NASA Goddard...
Main Author: | |
---|---|
Format: | Thesis |
Language: | English |
Published: |
2023
|
Subjects: | |
Online Access: | https://doi.org/10.7916/18qg-2y74 |
id |
ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/18qg-2y74 |
---|---|
record_format |
openpolar |
spelling |
ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/18qg-2y74 2023-09-26T15:21:10+02:00 Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing Mitevski, Ivan 2023 https://doi.org/10.7916/18qg-2y74 English eng https://doi.org/10.7916/18qg-2y74 Atmosphere Atmospheric carbon dioxide Meridional overturning circulation Ocean currents Ocean temperature Climatology Earth temperature Theses 2023 ftcolumbiauniv https://doi.org/10.7916/18qg-2y74 2023-08-26T22:20:54Z In this thesis, I explore the climate system's response to symmetric abrupt and transient CO₂ forcing across a range of concentrations, from ⅛ ⨉ to 8⨉CO₂, relative to pre-industrial levels. I use two CMIP6 class models: the CESM Large Ensemble (CESM-LE) model configuration and the NASA Goddard Institute for Space Studies Model E2.1-G (GISS-E2.1-G). I use a hierarchy of (1) fully coupled atmosphere-ocean-sea-ice-land, (2) slab ocean, and (3) prescribed sea surface temperature simulations to analyze and support the findings. First, I find an asymmetric response in global mean surface air temperature (????????_s) and effective climate sensitivity (EffCS) between colder and warmer experiments. The ????????_s response at 8⨉CO₂ is more than a third larger than the corresponding cooling at ⅛⨉CO₂. I attribute this assymetry primarily due to the non-logarithmic CO₂ forcing, not to changes in the radiative feedbacks. Second, I identify a non-monotonic response of EffCS in the warmer scenarios, with a minimum occurring at 4⨉CO₂ (3⨉CO₂) in CESM-LE (GISS-E2.1-G). This minimum in the warming simulations is associated with a non-monotonicity in the radiative feedback. Similar non-monotonic responses in Northern Hemisphere sea-ice, precipitation, the latitude of zero precipitation-minus-evaporation, and the strength of the Hadley cell are also identified. Comparing the climate response over the same CO₂ range between fully coupled and slab-ocean versions of the same models, I demonstrate that the climate system’s non-monotonic response is linked to changes in ocean dynamics, associated with a collapse of the Atlantic Meridional Overturning Circulation (AMOC). Third, to establish the significance of North Atlantic cooling in driving the non-monotonic changes in the radiative feedback, I conducted additional atmosphere-only (AMIP) simulations using the same models but with prescribed sea surface temperatures (SSTs) restricted to different regions. Through these simulations, I uncovered that the minimum EffCS value, characterized by notably ... Thesis North Atlantic Sea ice Columbia University: Academic Commons |
institution |
Open Polar |
collection |
Columbia University: Academic Commons |
op_collection_id |
ftcolumbiauniv |
language |
English |
topic |
Atmosphere Atmospheric carbon dioxide Meridional overturning circulation Ocean currents Ocean temperature Climatology Earth temperature |
spellingShingle |
Atmosphere Atmospheric carbon dioxide Meridional overturning circulation Ocean currents Ocean temperature Climatology Earth temperature Mitevski, Ivan Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
topic_facet |
Atmosphere Atmospheric carbon dioxide Meridional overturning circulation Ocean currents Ocean temperature Climatology Earth temperature |
description |
In this thesis, I explore the climate system's response to symmetric abrupt and transient CO₂ forcing across a range of concentrations, from ⅛ ⨉ to 8⨉CO₂, relative to pre-industrial levels. I use two CMIP6 class models: the CESM Large Ensemble (CESM-LE) model configuration and the NASA Goddard Institute for Space Studies Model E2.1-G (GISS-E2.1-G). I use a hierarchy of (1) fully coupled atmosphere-ocean-sea-ice-land, (2) slab ocean, and (3) prescribed sea surface temperature simulations to analyze and support the findings. First, I find an asymmetric response in global mean surface air temperature (????????_s) and effective climate sensitivity (EffCS) between colder and warmer experiments. The ????????_s response at 8⨉CO₂ is more than a third larger than the corresponding cooling at ⅛⨉CO₂. I attribute this assymetry primarily due to the non-logarithmic CO₂ forcing, not to changes in the radiative feedbacks. Second, I identify a non-monotonic response of EffCS in the warmer scenarios, with a minimum occurring at 4⨉CO₂ (3⨉CO₂) in CESM-LE (GISS-E2.1-G). This minimum in the warming simulations is associated with a non-monotonicity in the radiative feedback. Similar non-monotonic responses in Northern Hemisphere sea-ice, precipitation, the latitude of zero precipitation-minus-evaporation, and the strength of the Hadley cell are also identified. Comparing the climate response over the same CO₂ range between fully coupled and slab-ocean versions of the same models, I demonstrate that the climate system’s non-monotonic response is linked to changes in ocean dynamics, associated with a collapse of the Atlantic Meridional Overturning Circulation (AMOC). Third, to establish the significance of North Atlantic cooling in driving the non-monotonic changes in the radiative feedback, I conducted additional atmosphere-only (AMIP) simulations using the same models but with prescribed sea surface temperatures (SSTs) restricted to different regions. Through these simulations, I uncovered that the minimum EffCS value, characterized by notably ... |
format |
Thesis |
author |
Mitevski, Ivan |
author_facet |
Mitevski, Ivan |
author_sort |
Mitevski, Ivan |
title |
Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
title_short |
Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
title_full |
Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
title_fullStr |
Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
title_full_unstemmed |
Asymmetric and Non-monotonic Response of the Climate System to Idealized CO₂ Forcing |
title_sort |
asymmetric and non-monotonic response of the climate system to idealized co₂ forcing |
publishDate |
2023 |
url |
https://doi.org/10.7916/18qg-2y74 |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_relation |
https://doi.org/10.7916/18qg-2y74 |
op_doi |
https://doi.org/10.7916/18qg-2y74 |
_version_ |
1778145677080002560 |