Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming
The Paris Agreement has initiated a scientific debate on the role that carbon removal – or net negative emissions – might play in achieving less than 1.5 K of global mean surface warming by 2100. Here, we probe the sensitivity of a comprehensive Earth system model (GFDL-ESM2M) to three different atm...
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ftdoajarticles:oai:doaj.org/article:8b5ce7f23918432d8ca831c6bd6c4d1b 2023-05-15T17:36:55+02:00 Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming J. B. Palter T. L. Frölicher D. Paynter J. G. John 2018-06-01T00:00:00Z https://doi.org/10.5194/esd-9-817-2018 https://doaj.org/article/8b5ce7f23918432d8ca831c6bd6c4d1b EN eng Copernicus Publications https://www.earth-syst-dynam.net/9/817/2018/esd-9-817-2018.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-9-817-2018 2190-4979 2190-4987 https://doaj.org/article/8b5ce7f23918432d8ca831c6bd6c4d1b Earth System Dynamics, Vol 9, Pp 817-828 (2018) Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 article 2018 ftdoajarticles https://doi.org/10.5194/esd-9-817-2018 2023-01-08T01:38:38Z The Paris Agreement has initiated a scientific debate on the role that carbon removal – or net negative emissions – might play in achieving less than 1.5 K of global mean surface warming by 2100. Here, we probe the sensitivity of a comprehensive Earth system model (GFDL-ESM2M) to three different atmospheric CO 2 concentration pathways, two of which arrive at 1.5 K of warming in 2100 by very different pathways. We run five ensemble members of each of these simulations: (1) a standard Representative Concentration Pathway (RCP4.5) scenario, which produces 2 K of surface warming by 2100 in our model; (2) a <q>stabilization</q> pathway in which atmospheric CO 2 concentration never exceeds 440 ppm and the global mean temperature rise is approximately 1.5 K by 2100; and (3) an <q>overshoot</q> pathway that passes through 2 K of warming at mid-century, before ramping down atmospheric CO 2 concentrations, as if using carbon removal, to end at 1.5 K of warming at 2100. Although the global mean surface temperature change in response to the overshoot pathway is similar to the stabilization pathway in 2100, this similarity belies several important differences in other climate metrics, such as warming over land masses, the strength of the Atlantic Meridional Overturning Circulation (AMOC), ocean acidification, sea ice coverage, and the global mean sea level change and its regional expressions. In 2100, the overshoot ensemble shows a greater global steric sea level rise and weaker AMOC mass transport than in the stabilization scenario, with both of these metrics close to the ensemble mean of RCP4.5. There is strong ocean surface cooling in the North Atlantic Ocean and Southern Ocean in response to overshoot forcing due to perturbations in the ocean circulation. Thus, overshoot forcing in this model reduces the rate of sea ice loss in the Labrador, Nordic, Ross, and Weddell seas relative to the stabilized pathway, suggesting a negative radiative feedback in response to the early rapid warming. Finally, ... Article in Journal/Newspaper North Atlantic Ocean acidification Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Southern Ocean Weddell Earth System Dynamics 9 2 817 828 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
spellingShingle |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 J. B. Palter T. L. Frölicher D. Paynter J. G. John Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
topic_facet |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
description |
The Paris Agreement has initiated a scientific debate on the role that carbon removal – or net negative emissions – might play in achieving less than 1.5 K of global mean surface warming by 2100. Here, we probe the sensitivity of a comprehensive Earth system model (GFDL-ESM2M) to three different atmospheric CO 2 concentration pathways, two of which arrive at 1.5 K of warming in 2100 by very different pathways. We run five ensemble members of each of these simulations: (1) a standard Representative Concentration Pathway (RCP4.5) scenario, which produces 2 K of surface warming by 2100 in our model; (2) a <q>stabilization</q> pathway in which atmospheric CO 2 concentration never exceeds 440 ppm and the global mean temperature rise is approximately 1.5 K by 2100; and (3) an <q>overshoot</q> pathway that passes through 2 K of warming at mid-century, before ramping down atmospheric CO 2 concentrations, as if using carbon removal, to end at 1.5 K of warming at 2100. Although the global mean surface temperature change in response to the overshoot pathway is similar to the stabilization pathway in 2100, this similarity belies several important differences in other climate metrics, such as warming over land masses, the strength of the Atlantic Meridional Overturning Circulation (AMOC), ocean acidification, sea ice coverage, and the global mean sea level change and its regional expressions. In 2100, the overshoot ensemble shows a greater global steric sea level rise and weaker AMOC mass transport than in the stabilization scenario, with both of these metrics close to the ensemble mean of RCP4.5. There is strong ocean surface cooling in the North Atlantic Ocean and Southern Ocean in response to overshoot forcing due to perturbations in the ocean circulation. Thus, overshoot forcing in this model reduces the rate of sea ice loss in the Labrador, Nordic, Ross, and Weddell seas relative to the stabilized pathway, suggesting a negative radiative feedback in response to the early rapid warming. Finally, ... |
format |
Article in Journal/Newspaper |
author |
J. B. Palter T. L. Frölicher D. Paynter J. G. John |
author_facet |
J. B. Palter T. L. Frölicher D. Paynter J. G. John |
author_sort |
J. B. Palter |
title |
Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
title_short |
Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
title_full |
Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
title_fullStr |
Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
title_full_unstemmed |
Climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 K warming |
title_sort |
climate, ocean circulation, and sea level changes under stabilization and overshoot pathways to 1.5 k warming |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://doi.org/10.5194/esd-9-817-2018 https://doaj.org/article/8b5ce7f23918432d8ca831c6bd6c4d1b |
geographic |
Southern Ocean Weddell |
geographic_facet |
Southern Ocean Weddell |
genre |
North Atlantic Ocean acidification Sea ice Southern Ocean |
genre_facet |
North Atlantic Ocean acidification Sea ice Southern Ocean |
op_source |
Earth System Dynamics, Vol 9, Pp 817-828 (2018) |
op_relation |
https://www.earth-syst-dynam.net/9/817/2018/esd-9-817-2018.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-9-817-2018 2190-4979 2190-4987 https://doaj.org/article/8b5ce7f23918432d8ca831c6bd6c4d1b |
op_doi |
https://doi.org/10.5194/esd-9-817-2018 |
container_title |
Earth System Dynamics |
container_volume |
9 |
container_issue |
2 |
container_start_page |
817 |
op_container_end_page |
828 |
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1766136575538757632 |