Deep-ocean heat uptake and equilibrium climate response

We integrate the coupled climate model ECHAM5/MPIOM to equilibrium under atmospheric CO2 quadrupling. The equilibrium global-mean surface-temperature change is 10.8 K. The surface equilibrates within about 1,200 years, the deep ocean within 5,000 years. The impact of the deep ocean on the equilibriu...

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Published in:Climate Dynamics
Main Authors: Li, C., von Storch, J., Marotzke, J.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0012-3336-B
http://hdl.handle.net/11858/00-001M-0000-000E-C99E-F
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spelling ftpubman:oai:pure.mpg.de:item_1212585 2023-08-27T04:05:15+02:00 Deep-ocean heat uptake and equilibrium climate response Li, C. von Storch, J. Marotzke, J. 2013-03 application/pdf http://hdl.handle.net/11858/00-001M-0000-0012-3336-B http://hdl.handle.net/11858/00-001M-0000-000E-C99E-F eng eng info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-012-1350-z http://hdl.handle.net/11858/00-001M-0000-0012-3336-B http://hdl.handle.net/11858/00-001M-0000-000E-C99E-F Climate Dynamics info:eu-repo/semantics/article 2013 ftpubman https://doi.org/10.1007/s00382-012-1350-z 2023-08-02T01:39:15Z We integrate the coupled climate model ECHAM5/MPIOM to equilibrium under atmospheric CO2 quadrupling. The equilibrium global-mean surface-temperature change is 10.8 K. The surface equilibrates within about 1,200 years, the deep ocean within 5,000 years. The impact of the deep ocean on the equilibrium surface-temperature response is illustrated by the difference between ECHAM5/MPIOM and ECHAM5 coupled with slab ocean model (ECHAM5/SOM). The equilibrium global-mean surface temperature response is 11.1 K in ECHAM5/SOM and is thus 0.3 K higher than in ECHAM5/MPIOM. ECHAM5/MPIOM shows less warming over the northern-hemisphere mid and high latitudes, but larger warming over the tropical ocean and especially over the southern-hemisphere high latitudes. ECHAM5/MPIOM shows similar polar amplification in both the Arctic and the Antarctic, in contrast to ECHAM5/SOM, which shows stronger polar amplification in the northern hemisphere. The southern polar warming in ECHAM5/MPIOM is greatly delayed by Antarctic deep-ocean warming due to convective and isopycnal mixing. The equilibrium ocean temperature warming under CO2 quadrupling is around 8.0 K and is near-uniform with depth. The global-mean steric sea-level rise is 5.8 m in equilibrium; of this, 2.3 m are due to the deep-ocean warming after the surface temperature has almost equilibrated. This result suggests that the surface temperature change is a poor predictor for steric sea-level change in the long term. The effective climate response method described in Gregory et al. (2004) is evaluated with our simulation, which shows that their method to estimate the equilibrium climate response is accurate to within 10 %. Article in Journal/Newspaper Antarc* Antarctic Arctic Max Planck Society: MPG.PuRe Antarctic Arctic The Antarctic Climate Dynamics 40 5-6 1071 1086
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description We integrate the coupled climate model ECHAM5/MPIOM to equilibrium under atmospheric CO2 quadrupling. The equilibrium global-mean surface-temperature change is 10.8 K. The surface equilibrates within about 1,200 years, the deep ocean within 5,000 years. The impact of the deep ocean on the equilibrium surface-temperature response is illustrated by the difference between ECHAM5/MPIOM and ECHAM5 coupled with slab ocean model (ECHAM5/SOM). The equilibrium global-mean surface temperature response is 11.1 K in ECHAM5/SOM and is thus 0.3 K higher than in ECHAM5/MPIOM. ECHAM5/MPIOM shows less warming over the northern-hemisphere mid and high latitudes, but larger warming over the tropical ocean and especially over the southern-hemisphere high latitudes. ECHAM5/MPIOM shows similar polar amplification in both the Arctic and the Antarctic, in contrast to ECHAM5/SOM, which shows stronger polar amplification in the northern hemisphere. The southern polar warming in ECHAM5/MPIOM is greatly delayed by Antarctic deep-ocean warming due to convective and isopycnal mixing. The equilibrium ocean temperature warming under CO2 quadrupling is around 8.0 K and is near-uniform with depth. The global-mean steric sea-level rise is 5.8 m in equilibrium; of this, 2.3 m are due to the deep-ocean warming after the surface temperature has almost equilibrated. This result suggests that the surface temperature change is a poor predictor for steric sea-level change in the long term. The effective climate response method described in Gregory et al. (2004) is evaluated with our simulation, which shows that their method to estimate the equilibrium climate response is accurate to within 10 %.
format Article in Journal/Newspaper
author Li, C.
von Storch, J.
Marotzke, J.
spellingShingle Li, C.
von Storch, J.
Marotzke, J.
Deep-ocean heat uptake and equilibrium climate response
author_facet Li, C.
von Storch, J.
Marotzke, J.
author_sort Li, C.
title Deep-ocean heat uptake and equilibrium climate response
title_short Deep-ocean heat uptake and equilibrium climate response
title_full Deep-ocean heat uptake and equilibrium climate response
title_fullStr Deep-ocean heat uptake and equilibrium climate response
title_full_unstemmed Deep-ocean heat uptake and equilibrium climate response
title_sort deep-ocean heat uptake and equilibrium climate response
publishDate 2013
url http://hdl.handle.net/11858/00-001M-0000-0012-3336-B
http://hdl.handle.net/11858/00-001M-0000-000E-C99E-F
geographic Antarctic
Arctic
The Antarctic
geographic_facet Antarctic
Arctic
The Antarctic
genre Antarc*
Antarctic
Arctic
genre_facet Antarc*
Antarctic
Arctic
op_source Climate Dynamics
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-012-1350-z
http://hdl.handle.net/11858/00-001M-0000-0012-3336-B
http://hdl.handle.net/11858/00-001M-0000-000E-C99E-F
op_doi https://doi.org/10.1007/s00382-012-1350-z
container_title Climate Dynamics
container_volume 40
container_issue 5-6
container_start_page 1071
op_container_end_page 1086
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