Climate change, in the framework of the constructal law
Autor(a) principal: | |
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Data de Publicação: | 2011 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10174/3803 https://doi.org/10.5194/esdd-2-241-2011 |
Resumo: | Here we present a simple and transparent model of thermal behavior under time-changing conditions. We show the one-to-one relationship between changes in atmospheric properties and time-dependent changes in temperature and its distribution on Earth. The model accounts for convection and radiation, thermal inertia and changes in albedo () and greenhouse factor (). The constructal law is used as the principle that governs the evolution of flow configuration in time, and provides closure for the equations that describe the model. In the first part of the paper, the predictions are tested against the current thermal state of Earth. Next, the model showed that for two time-dependent scenarios, ( = 0.002 ; = 0.011) and ( = 0.002 ; = 0.005) the predicted equatorial and polar temperature increases and the time scales are (TH = 1.16 K ; TL = 1.11 K ; 104 years) and (0.41 K ; 0.41 K ; 57 years), respectively. In the second part, a continuous model of temperature variation was used to predict the thermal response of the Earth’s surface for changes bounded by = and . The results show that the global warming amplitudes and time scales are consistent with those obtained for = 0.002 and = 0.005. The poleward heat current reaches its maximum in the vicinity of 35° latitude, accounting for the position of the Ferrel cell between the Hadley and Polar Cells. |
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Climate change, in the framework of the constructal lawClimate ChangeConstructal lawHere we present a simple and transparent model of thermal behavior under time-changing conditions. We show the one-to-one relationship between changes in atmospheric properties and time-dependent changes in temperature and its distribution on Earth. The model accounts for convection and radiation, thermal inertia and changes in albedo () and greenhouse factor (). The constructal law is used as the principle that governs the evolution of flow configuration in time, and provides closure for the equations that describe the model. In the first part of the paper, the predictions are tested against the current thermal state of Earth. Next, the model showed that for two time-dependent scenarios, ( = 0.002 ; = 0.011) and ( = 0.002 ; = 0.005) the predicted equatorial and polar temperature increases and the time scales are (TH = 1.16 K ; TL = 1.11 K ; 104 years) and (0.41 K ; 0.41 K ; 57 years), respectively. In the second part, a continuous model of temperature variation was used to predict the thermal response of the Earth’s surface for changes bounded by = and . The results show that the global warming amplitudes and time scales are consistent with those obtained for = 0.002 and = 0.005. The poleward heat current reaches its maximum in the vicinity of 35° latitude, accounting for the position of the Ferrel cell between the Hadley and Polar Cells.2012-01-18T17:17:25Z2012-01-182011-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10174/3803http://hdl.handle.net/10174/3803https://doi.org/10.5194/esdd-2-241-2011engClausse, M.; Meunier, F.; Reis, A. H.; Bejan, A.Climate change, in the framework of the constructal law, Earth System Dynamics Discussions, 2, 1, 241-270, 2011.Departamento de Físicandndahr@uevora.ptnd242Clausse, M.Meunier, F.Reis, A. H.Bejan, A.info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T18:41:04Zoai:dspace.uevora.pt:10174/3803Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T00:59:06.769051Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Climate change, in the framework of the constructal law |
title |
Climate change, in the framework of the constructal law |
spellingShingle |
Climate change, in the framework of the constructal law Clausse, M. Climate Change Constructal law |
title_short |
Climate change, in the framework of the constructal law |
title_full |
Climate change, in the framework of the constructal law |
title_fullStr |
Climate change, in the framework of the constructal law |
title_full_unstemmed |
Climate change, in the framework of the constructal law |
title_sort |
Climate change, in the framework of the constructal law |
author |
Clausse, M. |
author_facet |
Clausse, M. Meunier, F. Reis, A. H. Bejan, A. |
author_role |
author |
author2 |
Meunier, F. Reis, A. H. Bejan, A. |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Clausse, M. Meunier, F. Reis, A. H. Bejan, A. |
dc.subject.por.fl_str_mv |
Climate Change Constructal law |
topic |
Climate Change Constructal law |
description |
Here we present a simple and transparent model of thermal behavior under time-changing conditions. We show the one-to-one relationship between changes in atmospheric properties and time-dependent changes in temperature and its distribution on Earth. The model accounts for convection and radiation, thermal inertia and changes in albedo () and greenhouse factor (). The constructal law is used as the principle that governs the evolution of flow configuration in time, and provides closure for the equations that describe the model. In the first part of the paper, the predictions are tested against the current thermal state of Earth. Next, the model showed that for two time-dependent scenarios, ( = 0.002 ; = 0.011) and ( = 0.002 ; = 0.005) the predicted equatorial and polar temperature increases and the time scales are (TH = 1.16 K ; TL = 1.11 K ; 104 years) and (0.41 K ; 0.41 K ; 57 years), respectively. In the second part, a continuous model of temperature variation was used to predict the thermal response of the Earth’s surface for changes bounded by = and . The results show that the global warming amplitudes and time scales are consistent with those obtained for = 0.002 and = 0.005. The poleward heat current reaches its maximum in the vicinity of 35° latitude, accounting for the position of the Ferrel cell between the Hadley and Polar Cells. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-01-01T00:00:00Z 2012-01-18T17:17:25Z 2012-01-18 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10174/3803 http://hdl.handle.net/10174/3803 https://doi.org/10.5194/esdd-2-241-2011 |
url |
http://hdl.handle.net/10174/3803 https://doi.org/10.5194/esdd-2-241-2011 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Clausse, M.; Meunier, F.; Reis, A. H.; Bejan, A.Climate change, in the framework of the constructal law, Earth System Dynamics Discussions, 2, 1, 241-270, 2011. Departamento de Física nd nd ahr@uevora.pt nd 242 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
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Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
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RCAAP |
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RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799136473796050944 |