An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models
An energy balance decomposition of temperature changes is conducted for idealized transient CO2-only simulations in the fifth phase of the Coupled Model Intercomparison Project. The multimodel global mean warming is dominated by enhanced clear-sky greenhouse effect due to increased CO2 and water vap...
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ftunivhelsihelda:oai:helda.helsinki.fi:10138/185058 2024-01-07T09:38:46+01:00 An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models Räisänen, Jouni Department of Physics 2017-05-17T06:04:03Z 14 application/pdf http://hdl.handle.net/10138/185058 eng eng Springer 10.1007/s00382-016-3277-2 We acknowledge the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for CMIP, and we thank the climate modeling groups for producing and making available their model output. For CMIP the U.S. Department of Energy's Program for Climate Model Diagnosis and Intercomparison provides coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. This work was supported by the Academy of Finland Centre of Excellence in Atmospheric Science-From Molecular and Biological processes to the Global Climate (project 272041). The two anonymous reviewers are acknowledged for their constructive comments. Räisänen , J 2017 , ' An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models ' , Climate dynamics : observational, theoretical and computational research on the climate system , vol. 48 , no. 9-10 , pp. 3441-3454 . https://doi.org/10.1007/s00382-016-3277-2 ORCID: /0000-0003-3657-1588/work/32700660 84982946466 1a906eb6-f354-46cd-b3a3-6bd13ad286ec http://hdl.handle.net/10138/185058 000399431900036 openAccess info:eu-repo/semantics/openAccess Temperature change Energy budget Atmospheric heat convergence Surface energy flux CMIP5 CLIMATE MODELS FEEDBACK SURFACE SIMULATIONS ADJUSTMENT SNOW CO2 114 Physical sciences Article acceptedVersion 2017 ftunivhelsihelda https://doi.org/10.1007/s00382-016-3277-2 2023-12-14T00:01:45Z An energy balance decomposition of temperature changes is conducted for idealized transient CO2-only simulations in the fifth phase of the Coupled Model Intercomparison Project. The multimodel global mean warming is dominated by enhanced clear-sky greenhouse effect due to increased CO2 and water vapour, but other components of the energy balance substantially modify the geographical and seasonal patterns of the change. Changes in the net surface energy flux are important over the oceans, being especially crucial for the muted warming over the northern North Atlantic and for the seasonal cycle of warming over the Arctic Ocean. Changes in atmospheric energy flux convergence tend to smooth the gradients of temperature change and reduce its land-sea contrast, but they also amplify the seasonal cycle of warming in northern North America and Eurasia. The three most important terms for intermodel differences in warming are the changes in the clear-sky greenhouse effect, clouds, and the net surface energy flux, making the largest contribution to the standard deviation of annual mean temperature change in 34, 29 and 20 % of the world, respectively. Changes in atmospheric energy flux convergence mostly damp intermodel variations of temperature change especially over the oceans. However, the opposite is true for example in Greenland and Antarctica, where the warming appears to be substantially controlled by heat transport from the surrounding sea areas. Peer reviewed Article in Journal/Newspaper Antarc* Antarctica Arctic Arctic Ocean Greenland North Atlantic HELDA – University of Helsinki Open Repository Arctic Arctic Ocean Greenland Climate Dynamics 48 9-10 3441 3454 |
institution |
Open Polar |
collection |
HELDA – University of Helsinki Open Repository |
op_collection_id |
ftunivhelsihelda |
language |
English |
topic |
Temperature change Energy budget Atmospheric heat convergence Surface energy flux CMIP5 CLIMATE MODELS FEEDBACK SURFACE SIMULATIONS ADJUSTMENT SNOW CO2 114 Physical sciences |
spellingShingle |
Temperature change Energy budget Atmospheric heat convergence Surface energy flux CMIP5 CLIMATE MODELS FEEDBACK SURFACE SIMULATIONS ADJUSTMENT SNOW CO2 114 Physical sciences Räisänen, Jouni An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
topic_facet |
Temperature change Energy budget Atmospheric heat convergence Surface energy flux CMIP5 CLIMATE MODELS FEEDBACK SURFACE SIMULATIONS ADJUSTMENT SNOW CO2 114 Physical sciences |
description |
An energy balance decomposition of temperature changes is conducted for idealized transient CO2-only simulations in the fifth phase of the Coupled Model Intercomparison Project. The multimodel global mean warming is dominated by enhanced clear-sky greenhouse effect due to increased CO2 and water vapour, but other components of the energy balance substantially modify the geographical and seasonal patterns of the change. Changes in the net surface energy flux are important over the oceans, being especially crucial for the muted warming over the northern North Atlantic and for the seasonal cycle of warming over the Arctic Ocean. Changes in atmospheric energy flux convergence tend to smooth the gradients of temperature change and reduce its land-sea contrast, but they also amplify the seasonal cycle of warming in northern North America and Eurasia. The three most important terms for intermodel differences in warming are the changes in the clear-sky greenhouse effect, clouds, and the net surface energy flux, making the largest contribution to the standard deviation of annual mean temperature change in 34, 29 and 20 % of the world, respectively. Changes in atmospheric energy flux convergence mostly damp intermodel variations of temperature change especially over the oceans. However, the opposite is true for example in Greenland and Antarctica, where the warming appears to be substantially controlled by heat transport from the surrounding sea areas. Peer reviewed |
author2 |
Department of Physics |
format |
Article in Journal/Newspaper |
author |
Räisänen, Jouni |
author_facet |
Räisänen, Jouni |
author_sort |
Räisänen, Jouni |
title |
An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
title_short |
An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
title_full |
An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
title_fullStr |
An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
title_full_unstemmed |
An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models |
title_sort |
energy balance perspective on regional co2-induced temperature changes in cmip5 models |
publisher |
Springer |
publishDate |
2017 |
url |
http://hdl.handle.net/10138/185058 |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Antarc* Antarctica Arctic Arctic Ocean Greenland North Atlantic |
genre_facet |
Antarc* Antarctica Arctic Arctic Ocean Greenland North Atlantic |
op_relation |
10.1007/s00382-016-3277-2 We acknowledge the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for CMIP, and we thank the climate modeling groups for producing and making available their model output. For CMIP the U.S. Department of Energy's Program for Climate Model Diagnosis and Intercomparison provides coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. This work was supported by the Academy of Finland Centre of Excellence in Atmospheric Science-From Molecular and Biological processes to the Global Climate (project 272041). The two anonymous reviewers are acknowledged for their constructive comments. Räisänen , J 2017 , ' An energy balance perspective on regional CO2-induced temperature changes in CMIP5 models ' , Climate dynamics : observational, theoretical and computational research on the climate system , vol. 48 , no. 9-10 , pp. 3441-3454 . https://doi.org/10.1007/s00382-016-3277-2 ORCID: /0000-0003-3657-1588/work/32700660 84982946466 1a906eb6-f354-46cd-b3a3-6bd13ad286ec http://hdl.handle.net/10138/185058 000399431900036 |
op_rights |
openAccess info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1007/s00382-016-3277-2 |
container_title |
Climate Dynamics |
container_volume |
48 |
container_issue |
9-10 |
container_start_page |
3441 |
op_container_end_page |
3454 |
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1787425640068153344 |