1. Identificação | |
Tipo de Referência | Artigo em Revista Científica (Journal Article) |
Site | mtc-m21b.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | 8JMKD3MGP5W34M/3FA4624 |
Repositório | sid.inpe.br/mtc-m21b/2013/11.26.17.01.32 |
Última Atualização | 2014:01.20.11.27.29 (UTC) administrator |
Repositório de Metadados | sid.inpe.br/mtc-m21b/2013/11.26.17.01.33 |
Última Atualização dos Metadados | 2018:06.04.03.14.13 (UTC) administrator |
DOI | 10.1175/JAS-D-12-0231.1 |
ISSN | 0022-4928 |
Rótulo | scopus 2013-11 |
Chave de Citação | MakarievaGoNeShNoBuLi:2013:KePhPa |
Título | The key physical parameters governing frictional dissipation in a precipitating atmosphere |
Ano | 2013 |
Data de Acesso | 18 maio 2024 |
Tipo Secundário | PRE PI |
Número de Arquivos | 1 |
Tamanho | 681 KiB |
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2. Contextualização | |
Autor | 1 Makarieva, A. M. 2 Gorshkov, V. G. 3 Nefiodov, A. V. 4 Sheil, D. 5 Nobre, Antonio Donato 6 Bunyard, P. 7 Li, B. -L. |
Grupo | 1 2 3 4 5 CST-CST-INPE-MCTI-GOV-BR |
Afiliação | 1 Theoretical Physics Division, Petersburg Nuclear Physics Institute, St. Petersburg, Russian Federation; XIEG-UCR International Center for Arid Land Ecology, University of California, Riverside, Riverside, CA, United States 2 Theoretical Physics Division, Petersburg Nuclear Physics Institute, St. Petersburg, Russian Federation 3 School of Environmental Science and Management, Southern Cross University, Lismore, NSW, Australia; Institute of Tropical Forest Conservation, Mbarara University of Science and Technology, P.O. Box 44, Kabale, Uganda; Center for International Forestry Research, Bogor, Indonesia 4 Centro de Ciência do Sistema Terrestre/INPE, São José dos Campos, São Paulo, Brazil 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 University Sergio Arboleda, Bogota, Colombia 7 XIEG-UCR International Center for Arid Land Ecology, University of California, Riverside, Riverside, CA, United States |
Endereço de e-Mail do Autor | 1 2 3 4 5 antonio.nobre@inpe.br |
Endereço de e-Mail | marcelo.pazos@inpe.br |
Revista | Journal of the Atmospheric Sciences |
Volume | 70 |
Número | 9 |
Páginas | 2916-2929 |
Nota Secundária | A1 A2 B1 |
Histórico (UTC) | 2018-06-04 03:14:13 :: administrator -> marcelo.pazos@inpe.br :: 2013 |
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3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Tipo de Versão | publisher |
Palavras-Chave | Atmosphere-land interactions Atmosphere-ocean interactions Atmospheric circulation Degree of condensation Frictional dissipation Hydrometeorology Physical parameters Surface temperatures Atmospheric temperature Climatology Condensation Estimation Friction Surface properties Turbulence Water vapor Tropics adiabatic process air temperature atmosphere-biosphere interaction atmosphere-hydrosphere interaction atmospheric circulation condensation hydrometeorology mixing ratio precipitation (climatology) relative humidity turbulence water vapor |
Resumo | Precipitation generates small-scale turbulent air flows-the energy of which ultimately dissipates to heat. The power of this process has previously been estimated to be around 2-4Wm-2 in the tropics: a value comparable in magnitude to the dynamic power of global atmospheric circulation. Here it is suggested that the true value is approximately half the value of this previous estimate. The result reflects a revised evaluation of the mean precipitation pathlength HP. The dependence of HP on surface temperature, relative humidity, temperature lapse rate, and degree of condensation in the ascending air were investigated. These analyses indicate that the degree of condensation, defined as the relative change of the saturated water vapor mixing ratio in the region of condensation, is a major factor determining HP. From this theory the authors develop an estimate indicating that the mean large-scale rate of frictional dissipation associated with total precipitation in the tropics lies between 1 and 2Wm-22 and show empirical evidence in support of this estimate. Under terrestrial conditions frictional dissipation is found to constitute a minor fraction of the dynamic power of condensation-induced atmospheric circulation, which is estimated to be at least 2.5 times larger. However, because HP increases with increasing surface temperature Ts, the rate of frictional dissipation would exceed the power of condensation-induced dynamics, and thus block major circulation, at Ts s 320K in a moist adiabatic atmosphere. © 2013 American Meteorological Society. |
Área | CST |
Arranjo | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > COCST > The key physical... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
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4. Condições de acesso e uso | |
URL dos dados | http://mtc-m21b.sid.inpe.br/ibi/8JMKD3MGP5W34M/3FA4624 |
URL dos dados zipados | http://mtc-m21b.sid.inpe.br/zip/8JMKD3MGP5W34M/3FA4624 |
Idioma | en |
Grupo de Usuários | administrator marcelo.pazos@inpe.br |
Grupo de Leitores | administrator marcelo.pazos@inpe.br |
Visibilidade | shown |
Política de Arquivamento | denypublisher6 allowfinaldraft |
Permissão de Leitura | allow from all |
Permissão de Atualização | não transferida |
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5. Fontes relacionadas | |
Repositório Espelho | iconet.com.br/banon/2006/11.26.21.31 |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3F3T29H |
Lista de Itens Citando | sid.inpe.br/bibdigital/2013/10.19.20.40 1 |
Divulgação | WEBSCI; SCOPUS. |
Acervo Hospedeiro | sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 |
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6. Notas | |
Campos Vazios | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject targetfile tertiarymark tertiarytype typeofwork url |
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7. Controle da descrição | |
e-Mail (login) | marcelo.pazos@inpe.br |
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